Veevers, John J; Heirtzler, James R (2005): Smear slide analysis of Hole 27-262 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230535
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
DSDP (1989): Data from the Deep Sea Drilling Project. Sediment, hard rock and reference files. National Geophysical Data Center, National Environmental Satellite, Data and Information Service, National Oceanic and Atmospheric Administration, U.S. Department of Commerce, 1, CD-ROM
Thayer, Paul A; Rocker, Karl; Robinson, Paul T; Renz, G W; Proto Decima, Franka; McKnight, Brian K; Krasheninnikov, Valery A; Cook, Peter J; Carter, Alan N; Bolli, Hans M; Veevers, John J; Heirtzler, James R (1974): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XXVII, 1060 pp, https://doi.org/10.2973/dsdp.proc.27.1974
Further details:
Processed smear slide data base - background and methods. hdl:10013/epic.32353.d001
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: -10.869800 * Longitude: 123.846300
Date/Time Start: 1972-11-24T00:00:00 * Date/Time End: 1972-11-24T00:00:00
Minimum DEPTH, sediment/rock: 2.55 m * Maximum DEPTH, sediment/rock: 434.10 m
Event(s):
27-262 * Latitude: -10.869800 * Longitude: 123.846300 * Date/Time: 1972-11-24T00:00:00 * Elevation: -2298.0 m * Penetration: 442 m * Recovery: 365.1 m * Location: Indian Ocean//TROUGH * Campaign: Leg27 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 47 cores; 442 m cored; 0 m drilled; 82.6 % recovery
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Sample code/label | Sample label | DSDP/ODP/IODP sample designation | |||
3 | Sand | Sand | % | Smear slide analysis | ||
4 | Silt | Silt | % | Smear slide analysis | ||
5 | Size fraction < 0.002 mm, clay | <2 µm | % | Smear slide analysis | ||
6 | Stratigraphy | Stratigraphy | Smear slide analysis | |||
7 | Lithology/composition/facies | Lithology | Smear slide analysis | |||
8 | Comment | Comment | Smear slide analysis | |||
9 | Carbonates | Carb | % | Smear slide analysis | ||
10 | Dolomite | Dol | % | Smear slide analysis | ||
11 | Nannofossils | Nannos | % | Smear slide analysis | ||
12 | Foraminifera | Foram | % | Smear slide analysis | ||
13 | Lamellibranchiata | Lamellibranchiata | % | Smear slide analysis | ||
14 | Calcareous spicules | Calc spic | % | Smear slide analysis | ||
15 | Ostracoda | Ostrac | % | Smear slide analysis | ||
16 | Chert | Chert | % | Smear slide analysis | fragments | |
17 | Radiolarians | Rad | % | Smear slide analysis | ||
18 | Diatoms | Diatoms | % | Smear slide analysis | ||
19 | Silicoflagellates | Silicoflag | % | Smear slide analysis | ||
20 | Spiculae | Spiculae | % | Smear slide analysis | ||
21 | Minerals, other | Min other | % | Smear slide analysis | ||
22 | Gypsum | Gp | % | Smear slide analysis | ||
23 | Quartz | Qz | % | Smear slide analysis | ||
24 | Feldspar | Fsp | % | Smear slide analysis | ||
25 | Zeolite | Zeo | % | Smear slide analysis | ||
26 | Mica | Mica | % | Smear slide analysis | ||
27 | Clay minerals | Clay min | % | Smear slide analysis | ||
28 | Glauconite | Glt | % | Smear slide analysis | ||
29 | Opaque minerals | Opaque | % | Smear slide analysis | ||
30 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
31 | Iron | Fe | % | Smear slide analysis | ||
32 | Heavy minerals | HM | % | Smear slide analysis | ||
33 | Zircon | Zrn | % | Smear slide analysis | ||
34 | Tourmaline | Tur | % | Smear slide analysis | ||
35 | Amphibole | Amp | % | Smear slide analysis | ||
36 | Pyroxene | Pyrox | % | Smear slide analysis | ||
37 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
38 | Rock fragments | Rock fragm | % | Smear slide analysis | ||
39 | Fragments, coal | Coal fragm | % | Smear slide analysis | carbon fragments | |
40 | Spherulite | Spherulite | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
13649 data points
Data
1 Depth sed [m] | 2 Sample label | 3 Sand [%] | 4 Silt [%] | 5 <2 µm [%] | 6 Stratigraphy | 7 Lithology | 8 Comment | 9 Carb [%] | 10 Dol [%] | 11 Nannos [%] | 12 Foram [%] | 13 Lamellibranchiata [%] | 14 Calc spic [%] | 15 Ostrac [%] | 16 Chert [%] | 17 Rad [%] | 18 Diatoms [%] | 19 Silicoflag [%] | 20 Spiculae [%] | 21 Min other [%] | 22 Gp [%] | 23 Qz [%] | 24 Fsp [%] | 25 Zeo [%] | 26 Mica [%] | 27 Clay min [%] | 28 Glt [%] | 29 Opaque [%] | 30 Py [%] | 31 Fe [%] | 32 HM [%] | 33 Zrn [%] | 34 Tur [%] | 35 Amp [%] | 36 Pyrox [%] | 37 Volc glass [%] | 38 Rock fragm [%] | 39 Coal fragm [%] | 40 Spherulite [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
2.55 | 27-262-1-21,105 | 10 | 30 | 60 | Quaternary | NANNO FORAM RICH CLAY | Minor lithology; relative abundance | 0 | 2 | 10 | 18 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 0 | 10 | 5 | 1 | 0 | 25 | 0 | 0 | 2 | 2 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 |
2.80 | 27-262-1-21,130 | 1 | 9 | 90 | Quaternary | FORAM CLAY BEARING NANNO OOZE | Dominat lithology; relative abundance | 10 | 2 | 65 | 2 | 0 | 0 | 0 | 0 | 10 | 2 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
4.20 | 27-262-1-31,120 | 1 | 80 | 19 | Quaternary | CLAY FORAM BEARING NANNO OOZE | Dominat lithology; relative abundance | 20 | 1 | 60 | 15 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 1 | 0 | 2 | 0 | 10 | 0 | 0 | 2 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
5.00 | 27-262-1-4,50 | 0 | 40 | 60 | Quaternary | FORAM BEARING CLAY NANNO OOZE | Dominat lithology; relative abundance | 30 | 2 | 34 | 5 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 1 | 0 | 2 | 0 | 25 | 0 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
5.50 | 27-262-1-41,100 | 30 | 70 | 0 | Pleistocene | FORAM SANDY SILT | Minor lithology; relative abundance | 20 | 2 | 0 | 68 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 1 | 0 | 0 | 5 | 0 | 0 | 2 | 0 | 0 | 23 | 2 | 0 | 3 | 2 | 2 | 23 | 23 | 0 | 0 | 0 | 0 |
5.80 | 27-262-1-41,130 | 0 | 90 | 10 | Pleistocene | FORAM CLAY BEARING NANNO OOZE | Dominat lithology; relative abundance | 5 | 1 | 60 | 5 | 0 | 0 | 0 | 0 | 5 | 1 | 2 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 10 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 |
6.10 | 27-262-1-CC,0 | 0 | 0 | 0 | Pleistocene | FORAM CLAY BEARING NANNO OOZE | Dominat lithology; relative abundance | 5 | 0 | 65 | 30 | 38 | 0 | 0 | 0 | 1 | 10 | 0 | 1 | 0 | 0 | 2 | 2 | 0 | 2 | 5 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 2 |
6.10 | 27-262-1-CC,0 | 100 | 0 | 0 | Pleistocene | FORAM CLAY BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 15 | 2 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
6.10 | 27-262-1-CC,0 | 100 | 0 | 0 | Pleistocene | FORAM CLAY-BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 60 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
6.39 | 27-262-2-11,139 | 0 | 80 | 20 | Pleistocene | CLAY DOLO BEARING FORAM NANNO OOZE | Dominat lithology; relative abundance | 25 | 2 | 64 | 5 | 0 | 0 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
7.25 | 27-262-2-2,75 | 10 | 70 | 20 | Pleistocene | CLAY BEARING FORAM RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 43 | 10 | 0 | 0 | 0 | 0 | 20 | 2 | 1 | 2 | 0 | 0 | 2 | 0 | 2 | 2 | 5 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 |
8.75 | 27-262-2-3,75 | 0 | 0 | 0 | Pleistocene | RAD RICH CLAY NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 36 | 3 | 0 | 0 | 0 | 0 | 20 | 1 | 2 | 2 | 0 | 0 | 2 | 0 | 2 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 3 | 0 |
10.25 | 27-262-2-4,75 | 0 | 30 | 70 | Pleistocene | FORAM BEARING CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 45 | 5 | 0 | 0 | 0 | 0 | 10 | 2 | 1 | 2 | 0 | 0 | 1 | 2 | 0 | 0 | 15 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 10 | 0 |
11.10 | 27-262-2-CC,0 | 0 | 0 | 0 | Pleistocene | CLAY BEARING RAD RICH NANNO OOZE | Dominat lithology; numerical abundance | 0 | 1 | 67 | 10 | 2 | 0 | 0 | 0 | 15 | 10 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 5 | 0 | 0 | 15 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 |
11.10 | 27-262-2-CC,0 | 100 | 0 | 0 | Pleistocene | CLAY BEARING RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 73 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
11.10 | 27-262-2-CC,0 | 100 | 40 | 60 | Pleistocene | CLAY BEARING RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 85 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
16.75 | 27-262-3-2,75 | 0 | 80 | 20 | Pleistocene | CLAY FORAM BEARING RAD NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 68 | 5 | 0 | 0 | 0 | 0 | 10 | 2 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 5 | 0 | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
18.25 | 27-262-3-3,75 | 5 | 40 | 55 | Pleistocene | FORAM BEARING CLAY RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 36 | 10 | 0 | 0 | 0 | 0 | 20 | 3 | 0 | 0 | 0 | 0 | 2 | 0 | 1 | 0 | 15 | 0 | 0 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 10 | 0 |
19.70 | 27-262-3-4,70 | 0 | 70 | 30 | Pleistocene | FORAM DIATOM BEARING RAD NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 70 | 3 | 0 | 0 | 1 | 0 | 10 | 3 | 1 | 1 | 0 | 0 | 1 | 0 | 2 | 0 | 2 | 0 | 0 | 3 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 |
20.05 | 27-262-3-41,104.5 | 0 | 60 | 40 | Pleistocene | PYRITIC CLAY FORAM RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 70 | 5 | 0 | 0 | 0 | 0 | 10 | 1 | 2 | 1 | 0 | 0 | 1 | 0 | 1 | 0 | 5 | 0 | 0 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
21.39 | 27-262-3-5,89 | 5 | 45 | 50 | Pleistocene | RAD BEARING FORAM CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 46 | 15 | 0 | 0 | 0 | 0 | 5 | 2 | 1 | 1 | 0 | 0 | 1 | 0 | 1 | 0 | 20 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
22.71 | 27-262-3-6,71 | 0 | 30 | 70 | Pleistocene | RAD CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 46 | 5 | 0 | 0 | 0 | 0 | 15 | 2 | 1 | 1 | 0 | 0 | 1 | 0 | 1 | 0 | 20 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
22.89 | 27-262-3-6,89 | 0 | 20 | 80 | Pleistocene | PYRITIC RAD BEARING NANNO CLAY | Minor lithology; relative abundance | 0 | 0 | 30 | 3 | 0 | 0 | 0 | 0 | 10 | 1 | 2 | 1 | 0 | 0 | 2 | 2 | 0 | 0 | 40 | 0 | 0 | 5 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
23.60 | 27-262-3-CC,0 | 100 | 0 | 0 | Pleistocene | CLAY FORAM BEARING RAD RICH NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 68 | 1 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
23.60 | 27-262-3-CC,0 | 100 | 0 | 0 | Pleistocene | CLAY FORAM BEARING RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 25 | 0 | 0 | 0 | 0 | 75 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
23.60 | 27-262-3-CC,0 | 0 | 80 | 20 | Pleistocene | CLAY FORAM BEARING RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 47 | 5 | 0 | 0 | 0 | 0 | 15 | 1 | 2 | 2 | 0 | 0 | 1 | 1 | 2 | 0 | 10 | 0 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 |
25.00 | 27-262-4-11,100 | 1 | 15 | 84 | Pleistocene | PYRITIC FORAM RAD NANNO BEARING CLAY | Dominat lithology; relative abundance | 0 | 1 | 11 | 3 | 0 | 0 | 0 | 0 | 10 | 1 | 2 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 50 | 0 | 0 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 |
26.40 | 27-262-4-2,90 | 0 | 20 | 80 | Pleistocene | FORAM RAD BEARING NANNO RICH CLAY | Dominat lithology; relative abundance | 0 | 1 | 16 | 5 | 0 | 0 | 0 | 1 | 10 | 1 | 2 | 1 | 0 | 0 | 1 | 2 | 1 | 0 | 50 | 0 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 10 | 0 |
27.90 | 27-262-4-3,90 | 10 | 10 | 80 | Pleistocene | FORAM NANNO BEARING RAD RICH CLAY | Dominat lithology; relative abundance | 0 | 1 | 10 | 5 | 0 | 0 | 0 | 0 | 15 | 1 | 2 | 1 | 0 | 0 | 2 | 0 | 1 | 0 | 40 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 |
29.50 | 27-262-4-41,100 | 5 | 25 | 70 | Pleistocene | DETRITAL FORAM BEARING CLAY NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 46 | 10 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 3 | 0 | 0 | 2 | 1 | 1 | 0 | 30 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 |
30.10 | 27-262-4-CC,0 | 0 | 0 | 0 | Pleistocene | RAD CLAY BEARING NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 46 | 1 | 0 | 0 | 0 | 35 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
30.10 | 27-262-4-CC,0 | 100 | 0 | 0 | Pleistocene | RAD CLAY BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 60 | 0 | 0 | 0 | 0 | 46 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
30.10 | 27-262-4-CC,0 | 5 | 45 | 50 | Pleistocene | RAD CLAY BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 49 | 3 | 0 | 0 | 0 | 0 | 10 | 2 | 2 | 1 | 0 | 0 | 5 | 1 | 2 | 0 | 10 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 |
34.50 | 27-262-5-11,100 | 1 | 29 | 70 | Pleistocene | DETRITAL FORAM BEARING RAD RICH CLAY NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 33 | 5 | 0 | 0 | 0 | 0 | 15 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 2 | 0 | 30 | 0 | 0 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 1 | 0 | 10 | 0 |
37.25 | 27-262-5-3,75 | 1 | 50 | 49 | Pleistocene | DETRITAL FORAM BEARING CLAY RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 44 | 5 | 0 | 0 | 0 | 0 | 15 | 2 | 0 | 2 | 0 | 0 | 2 | 0 | 2 | 0 | 15 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 |
38.75 | 27-262-5-4,75 | 0 | 30 | 70 | Pleistocene | RAD RICH CLAY NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 29 | 2 | 0 | 0 | 0 | 0 | 20 | 2 | 2 | 1 | 0 | 0 | 3 | 0 | 1 | 0 | 30 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 10 | 0 |
40.25 | 27-262-5-5,75 | 5 | 20 | 75 | Pleistocene | FORAM RAD BEARING NANNO OOZE | Dominat lithology; numerical abundance | 0 | 2 | 31 | 5 | 0 | 0 | 0 | 0 | 15 | 5 | 0 | 1 | 0 | 0 | 1 | 0 | 1 | 0 | 40 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 |
41.75 | 27-262-5-6,75 | 0 | 40 | 60 | Pleistocene | FORAM RAD BEARING CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 29 | 0 | 0 | 0 | 0 | 0 | 20 | 5 | 2 | 1 | 0 | 0 | 2 | 0 | 1 | 0 | 30 | 0 | 0 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
42.60 | 27-262-5-CC,0 | 100 | 0 | 0 | Pleistocene | FORAM DIATOM CLAY BEARING RAD RICH NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 60 | 2 | 0 | 0 | 0 | 30 | 1 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
42.60 | 27-262-5-CC,0 | 100 | 0 | 0 | Pleistocene | FORAM DIATOM CLAY BEARING RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 60 | 0 | 0 | 0 | 0 | 36 | 2 | 0 | 7 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
42.60 | 27-262-5-CC,0 | 0 | 50 | 50 | Pleistocene | FORAM DIATOM CLAY BEARING RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 5 | 0 | 50 | 5 | 0 | 0 | 0 | 0 | 20 | 5 | 0 | 2 | 0 | 0 | 5 | 1 | 1 | 0 | 5 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
44.10 | 27-262-6-1,80 | 10 | 70 | 20 | Pleistocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 2 | 42 | 5 | 0 | 0 | 2 | 0 | 25 | 3 | 0 | 1 | 0 | 0 | 2 | 0 | 2 | 0 | 15 | 0 | 0 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 |
45.55 | 27-262-6-2,75 | 1 | 90 | 9 | Pleistocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 36 | 3 | 0 | 0 | 0 | 0 | 15 | 2 | 2 | 1 | 0 | 0 | 2 | 0 | 1 | 0 | 30 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 7 | 0 |
46.25 | 27-262-6-21,145 | 30 | 70 | 0 | Pleistocene | SANDY SILT | Minor lithology; relative abundance | 0 | 1 | 10 | 25 | 0 | 0 | 0 | 10 | 1 | 2 | 0 | 2 | 0 | 0 | 7 | 7 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 35 | 0 |
47.00 | 27-262-6-3,70 | 0 | 80 | 20 | Pleistocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 15 | 1 | 1 | 2 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
48.60 | 27-262-6-4,80 | 5 | 90 | 5 | Pleistocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 2 | 0 | 2 | 0 | 0 | 2 | 0 | 20 | 3 | 2 | 1 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 |
50.10 | 27-262-6-5,80 | 5 | 75 | 20 | Pleistocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 5 | 2 | 2 | 1 | 0 | 0 | 2 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
51.55 | 27-262-6-6,75 | 5 | 75 | 20 | Pleistocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 5 | 2 | 2 | 1 | 0 | 0 | 2 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
52.40 | 27-262-6-CC,0 | 100 | 0 | 0 | Pleistocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 45 | 0 | 0 | 0 | 0 | 45 | 4 | 0 | 5 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
52.40 | 27-262-6-CC,0 | 1 | 80 | 19 | Pleistocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 5 | 0 | 0 | 2 | 0 | 10 | 1 | 2 | 1 | 0 | 0 | 2 | 1 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 |
53.70 | 27-262-7-1,70 | 0 | 40 | 60 | Pleistocene | FORAM CLAY RAD BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 56 | 1 | 0 | 0 | 0 | 0 | 15 | 1 | 2 | 2 | 0 | 0 | 1 | 1 | 2 | 0 | 10 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
57.00 | 27-262-7-31,100 | 0 | 40 | 60 | Pleistocene | FORAM CLAY RAD BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 56 | 1 | 0 | 0 | 0 | 0 | 15 | 1 | 2 | 2 | 0 | 0 | 1 | 1 | 2 | 0 | 10 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
58.10 | 27-262-7-4,60 | 0 | 40 | 60 | Pleistocene | FORAM CLAY RAD BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 61 | 1 | 0 | 0 | 0 | 0 | 10 | 2 | 2 | 2 | 0 | 0 | 1 | 1 | 2 | 0 | 10 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
59.75 | 27-262-7-5,75 | 0 | 15 | 85 | Pleistocene | DETRITAL FORAM BEARING RAD CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 22 | 5 | 0 | 0 | 2 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 5 | 0 | 2 | 0 | 25 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
62.10 | 27-262-7-CC,0 | 100 | 0 | 0 | Pleistocene | CLAY RAD BEARING NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 15 | 1 | 0 | 0 | 0 | 38 | 2 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
62.10 | 27-262-7-CC,0 | 100 | 0 | 0 | Pleistocene | CLAY RAD BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 50 | 0 | 0 | 0 | 0 | 64 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
62.10 | 27-262-7-CC,0 | 0 | 30 | 70 | Pleistocene | CLAY RAD BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 62 | 2 | 0 | 0 | 0 | 0 | 10 | 2 | 0 | 1 | 0 | 0 | 1 | 0 | 1 | 0 | 5 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 15 | 0 |
63.20 | 27-262-8-1,70 | 0 | 20 | 80 | Pleistocene | FORAM RAD BEARING CLAY NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 31 | 2 | 0 | 0 | 0 | 0 | 5 | 2 | 2 | 2 | 0 | 0 | 2 | 0 | 1 | 0 | 35 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 |
66.25 | 27-262-8-3,75 | 0 | 50 | 50 | Pleistocene | FORAM DIATOM BEARING CLAY RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 52 | 2 | 0 | 0 | 0 | 0 | 20 | 3 | 2 | 2 | 0 | 0 | 2 | 0 | 1 | 0 | 2 | 0 | 0 | 2 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
67.75 | 27-262-8-4,75 | 0 | 50 | 50 | Pleistocene | CLAY BEARING RAD NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 34 | 2 | 0 | 0 | 0 | 0 | 25 | 3 | 1 | 1 | 0 | 0 | 2 | 0 | 2 | 0 | 10 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 |
70.80 | 27-262-8-6,80 | 5 | 20 | 75 | Pleistocene | FORAM BEARING RAD RICH NANNO CLAY | Dominat lithology; relative abundance | 0 | 1 | 28 | 4 | 0 | 0 | 0 | 0 | 15 | 2 | 2 | 1 | 0 | 0 | 2 | 0 | 1 | 0 | 30 | 0 | 0 | 1 | 2 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 15 | 0 |
72.30 | 27-262-8-7,80 | 5 | 20 | 75 | Pleistocene | FORAM BEARING RAD RICH NANNO CLAY | Dominat lithology; relative abundance | 0 | 1 | 28 | 4 | 0 | 0 | 0 | 0 | 15 | 2 | 2 | 1 | 0 | 0 | 2 | 0 | 1 | 0 | 30 | 0 | 0 | 1 | 2 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 15 | 0 |
72.80 | 27-262-9-1,80 | 0 | 50 | 50 | Pleistocene | DIATOM CLAY BEARING RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 59 | 1 | 0 | 0 | 2 | 0 | 25 | 3 | 2 | 2 | 0 | 0 | 2 | 0 | 1 | 0 | 5 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 |
73.30 | 27-262-8-8,30 | 5 | 20 | 75 | Pleistocene | RAD RICH CLAY NANNO OOZE | Minor lithology; relative abundance | 10 | 2 | 39 | 2 | 0 | 0 | 0 | 0 | 15 | 1 | 2 | 2 | 0 | 0 | 1 | 0 | 1 | 0 | 30 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
73.56 | 27-262-8-8,56 | 10 | 70 | 20 | Pleistocene | CLAY FORAM RAD BEARING NANNO OOZE | Minor lithology; relative abundance | 0 | 0 | 53 | 5 | 0 | 0 | 0 | 0 | 10 | 1 | 2 | 2 | 0 | 0 | 1 | 2 | 2 | 0 | 5 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 1 | 0 | 20 | 0 |
73.77 | 27-262-8-8,77 | 80 | 20 | 0 | Pleistocene | NANNO RAD BEARING DETRITAL FORAM SAND | Dominat lithology; relative abundance | 0 | 0 | 0 | 77 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
74.10 | 27-262-9-2,60 | 0 | 50 | 50 | Pleistocene | DIATOM CLAY BEARING RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 54 | 1 | 0 | 0 | 2 | 0 | 25 | 3 | 2 | 2 | 0 | 0 | 2 | 0 | 1 | 0 | 10 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 |
74.60 | 27-262-8-CC,0 | 100 | 0 | 0 | Pleistocene | RAD NANNO RICH DETRITAL FORAM SANDY SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 45 | 0 | 2 | 0 | 0 | 10 | 10 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
74.60 | 27-262-8-CC,0 | 100 | 0 | 0 | Pleistocene | RAD NANNO RICH DETRITAL FORAM SANDY SILT | Dominat lithology; relative abundance | 0 | 0 | 0 | 68 | 0 | 20 | 0 | 0 | 40 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
75.80 | 27-262-9-3,80 | 0 | 50 | 50 | Pleistocene | DIATOM CLAY BEARING RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 59 | 1 | 0 | 0 | 2 | 0 | 25 | 3 | 2 | 2 | 0 | 0 | 2 | 0 | 1 | 0 | 5 | 2 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 |
77.30 | 27-262-9-4,80 | 0 | 50 | 50 | Pleistocene | DIATOM CLAY BEARING RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 59 | 1 | 0 | 0 | 2 | 0 | 25 | 5 | 2 | 2 | 0 | 0 | 2 | 0 | 1 | 0 | 5 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 |
78.80 | 27-262-9-5,80 | 2 | 48 | 50 | Pleistocene | FORAM RAD CLAY BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 53 | 5 | 0 | 0 | 0 | 0 | 10 | 1 | 2 | 1 | 0 | 0 | 1 | 0 | 1 | 0 | 10 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 15 | 0 |
80.50 | 27-262-9-61,100 | 3 | 50 | 47 | Pleistocene | DIATOM CLAY BEARING RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 60 | 2 | 0 | 0 | 0 | 0 | 15 | 3 | 2 | 1 | 0 | 0 | 2 | 0 | 1 | 0 | 5 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 10 | 0 |
81.10 | 27-262-9-CC,0 | 100 | 0 | 0 | Pleistocene | SILTY CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 48 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
81.10 | 27-262-9-CC,0 | 100 | 0 | 0 | Pleistocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 45 | 0 | 0 | 0 | 0 | 75 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
82.29 | 27-262-10-1,75 | 5 | 10 | 85 | Pleistocene | RAD DETRITAL FORAM RICH CLAY NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 44 | 10 | 0 | 0 | 0 | 0 | 10 | 2 | 2 | 1 | 0 | 0 | 1 | 0 | 1 | 0 | 25 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
83.79 | 27-262-10-2,75 | 2 | 48 | 50 | Pleistocene | FORAM CLAY BEARING RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 58 | 5 | 0 | 0 | 0 | 0 | 15 | 3 | 2 | 1 | 0 | 0 | 1 | 0 | 1 | 0 | 10 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 |
85.34 | 27-262-10-3,80 | 2 | 40 | 58 | Pleistocene | RAD CLAY NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 29 | 2 | 0 | 0 | 0 | 0 | 25 | 2 | 2 | 2 | 0 | 0 | 2 | 0 | 1 | 0 | 25 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 15 | 0 |
86.94 | 27-262-10-4,90 | 2 | 40 | 58 | Pleistocene | RAD CLAY NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 29 | 2 | 0 | 0 | 0 | 0 | 25 | 2 | 2 | 2 | 0 | 0 | 2 | 0 | 1 | 0 | 25 | 2 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 15 | 0 |
88.20 | 27-262-10-5,66 | 70 | 30 | 0 | Pleistocene | NANNO BEARING DETRITAL FORAM SILTY SAND | Minor lithology; relative abundance | 0 | 0 | 5 | 84 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
89.84 | 27-262-10-6,80 | 2 | 60 | 38 | Pleistocene | FORAM BEARING RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 75 | 3 | 0 | 0 | 0 | 0 | 10 | 2 | 2 | 1 | 0 | 0 | 1 | 2 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 |
90.64 | 27-262-10-CC,0 | 100 | 0 | 0 | Pleistocene | SILTY CLAY | Dominat lithology; relative abundance | 20 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 30 | 10 | 2 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
90.64 | 27-262-10-CC,0 | 100 | 0 | 0 | Pleistocene | SILTY CLAY | Dominat lithology; relative abundance | 3 | 0 | 0 | 45 | 0 | 0 | 0 | 0 | 33 | 0 | 2 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
91.80 | 27-262-11-1,80 | 2 | 60 | 38 | Pleistocene | FORAM BEARING RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 75 | 3 | 0 | 0 | 0 | 0 | 10 | 2 | 2 | 1 | 0 | 0 | 1 | 2 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 |
93.10 | 27-262-11-2,60 | 2 | 30 | 68 | Pleistocene | FORAM BEARING CLAY RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 50 | 3 | 0 | 0 | 0 | 0 | 20 | 2 | 2 | 1 | 0 | 0 | 1 | 0 | 1 | 0 | 15 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 |
95.05 | 27-262-11-31,105 | 2 | 50 | 48 | Pleistocene | FORAM CLAY RAD BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 73 | 2 | 0 | 0 | 0 | 0 | 10 | 1 | 2 | 1 | 0 | 0 | 1 | 0 | 1 | 0 | 5 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 |
96.40 | 27-262-11-4,90 | 2 | 50 | 48 | Pleistocene | DETRITAL-FORAM CLAY BEARING RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 48 | 5 | 0 | 0 | 1 | 0 | 20 | 2 | 2 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
97.80 | 27-262-11-5,80 | 2 | 50 | 48 | Pleistocene | DETRITAL FORAM CLAY BEARING RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 43 | 5 | 0 | 0 | 1 | 0 | 20 | 2 | 2 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 15 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
99.29 | 27-262-11-6,79 | 2 | 60 | 38 | Pleistocene | FORAM CLAY BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 65 | 5 | 0 | 0 | 0 | 0 | 2 | 1 | 2 | 2 | 0 | 0 | 3 | 2 | 1 | 0 | 10 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 20 | 0 |
99.74 | 27-262-11-61,124 | 60 | 40 | 0 | Pleistocene | RAD NANNO BEARING DETRITAL FORAM SILTY SAND | Minor lithology; relative abundance | 0 | 0 | 10 | 5 | 0 | 0 | 0 | 0 | 3 | 2 | 0 | 1 | 0 | 0 | 4 | 3 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
100.10 | 27-262-11-CC,0 | 100 | 0 | 0 | Pleistocene | FORAM CLAY BEARING NANNO OOZE | Dominat lithology; numerical abundance | 10 | 0 | 0 | 35 | 0 | 0 | 0 | 0 | 35 | 15 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
100.10 | 27-262-11-CC,0 | 100 | 0 | 0 | Pleistocene | FORAM CLAY BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 50 | 0 | 0 | 0 | 0 | 45 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
100.10 | 27-262-11-CC,0 | 2 | 60 | 38 | Pleistocene | FORAM CLAY BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 65 | 5 | 0 | 0 | 0 | 0 | 2 | 11 | 2 | 2 | 0 | 0 | 3 | 2 | 1 | 0 | 10 | 0 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 20 | 0 |
102.00 | 27-262-12-11,120 | 2 | 60 | 38 | Pleistocene | FORAM CLAY BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 65 | 5 | 0 | 0 | 0 | 0 | 2 | 1 | 2 | 2 | 0 | 0 | 3 | 2 | 1 | 0 | 10 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 20 | 0 |
103.20 | 27-262-12-2,90 | 70 | 20 | 5 | Pleistocene | NANNO RICH DETRITAL FORAM SILTY SAND | Dominat lithology; relative abundance | 0 | 0 | 26 | 50 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 |
104.50 | 27-262-12-3,70 | 80 | 5 | 15 | Pleistocene | NANNO BEARING DETRITAL FORAM SAND | Dominat lithology; relative abundance | 10 | 2 | 15 | 69 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 1 | 0 | 0 | 2 | 2 | 2 | 0 | 0 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
106.30 | 27-262-12-41,100 | 70 | 15 | 10 | Pleistocene | NANNO RICH FORAM BEARING SILTY SAND | Dominat lithology; relative abundance | 0 | 0 | 25 | 56 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 |
107.70 | 27-262-12-5,90 | 30 | 60 | 10 | Pleistocene | CLAY BEARING NANNO RICH DETRITAL QUARTZ FORAM SANDY SILT | Dominat lithology; relative abundance | 0 | 2 | 20 | 35 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 0 | 20 | 0 | 0 | 0 | 5 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 |
109.05 | 27-262-12-6,75 | 1 | 60 | 39 | Pleistocene | DIATOM CLAY RAD BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 65 | 2 | 0 | 0 | 0 | 0 | 5 | 3 | 0 | 2 | 0 | 0 | 1 | 1 | 1 | 1 | 5 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 1 | 0 | 15 | 0 |
109.90 | 27-262-12-CC,0 | 1 | 0 | 0 | Pleistocene | FORAM BEARING CLAY RICH NANNO OOZE | Dominat lithology; numerical abundance | 15 | 0 | 53 | 10 | 0 | 6 | 0 | 0 | 2 | 1 | 2 | 2 | 0 | 0 | 2 | 0 | 2 | 0 | 15 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
109.90 | 27-262-12-CC,0 | 100 | 0 | 0 | Pleistocene | FORAM BEARING CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 20 | 0 | 0 | 45 | 0 | 0 | 0 | 0 | 25 | 5 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
109.90 | 27-262-12-CC,0 | 100 | 49 | 50 | Pleistocene | FORAM BEARING CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 5 | 0 | 0 | 50 | 0 | 0 | 0 | 0 | 34 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
110.80 | 27-262-13-1,80 | 0 | 40 | 60 | Pleistocene | FORAM DIATOM BEARING CLAY RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 33 | 5 | 0 | 0 | 0 | 0 | 20 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 1 | 0 | 20 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 15 | 0 |
112.25 | 27-262-13-2,75 | 0 | 40 | 60 | Pleistocene | FORAM DIATOM BEARING CLAY RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 48 | 5 | 0 | 0 | 0 | 0 | 20 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 1 | 0 | 5 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 15 | 0 |
114.00 | 27-262-13-31,100 | 0 | 40 | 60 | Pleistocene | FORAM DIATOM BEARING CLAY RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 33 | 5 | 0 | 0 | 0 | 0 | 20 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 1 | 0 | 20 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 15 | 0 |
115.40 | 27-262-13-4,90 | 0 | 30 | 70 | Pleistocene | DIATOM BEARING RAD RICH CLAY NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 35 | 2 | 0 | 0 | 0 | 0 | 20 | 5 | 2 | 1 | 0 | 0 | 2 | 0 | 1 | 0 | 25 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
117.00 | 27-262-13-51,100 | 0 | 30 | 70 | Pleistocene | DIATOM BEARING RAD RICH CLAY NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 35 | 2 | 0 | 0 | 0 | 0 | 20 | 5 | 2 | 1 | 0 | 0 | 1 | 0 | 2 | 0 | 25 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
118.30 | 27-262-13-6,80 | 0 | 30 | 70 | Pleistocene | DIATOM BEARING RAD RICH CLAY NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 35 | 2 | 0 | 0 | 0 | 0 | 25 | 3 | 2 | 1 | 0 | 0 | 1 | 0 | 2 | 0 | 25 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
119.10 | 27-262-13-CC,0 | 100 | 0 | 0 | Pleistocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 45 | 3 | 0 | 0 | 0 | 25 | 2 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
119.10 | 27-262-13-CC,0 | 100 | 0 | 0 | Pleistocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 50 | 0 | 0 | 0 | 0 | 40 | 0 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
119.50 | 27-262-14-1,0 | 0 | 60 | 40 | Pleistocene | RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 70 | 3 | 0 | 0 | 0 | 0 | 15 | 2 | 2 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 |
121.75 | 27-262-14-2,75 | 0 | 60 | 40 | Pleistocene | FORAM BEARING CLAY RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 62 | 3 | 0 | 0 | 0 | 0 | 15 | 1 | 2 | 1 | 0 | 0 | 2 | 0 | 2 | 0 | 10 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
123.25 | 27-262-14-3,75 | 0 | 20 | 80 | Pleistocene | RAD RICH CLAY NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 45 | 2 | 0 | 0 | 0 | 0 | 15 | 2 | 0 | 1 | 0 | 0 | 2 | 0 | 1 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 |
124.75 | 27-262-14-4,75 | 0 | 50 | 50 | Pleistocene | FORAM CLAY BEARING RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 6 | 5 | 0 | 0 | 0 | 0 | 20 | 1 | 2 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 5 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 |
126.20 | 27-262-14-5,70 | 0 | 0 | 0 | Pleistocene | RAD BEARING CLAY NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 40 | 1 | 0 | 0 | 2 | 0 | 20 | 1 | 2 | 1 | 0 | 0 | 2 | 0 | 2 | 0 | 25 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 10 | 0 |
127.75 | 27-262-14-6,75 | 0 | 70 | 30 | Pleistocene | CLAY BEARING RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 59 | 2 | 0 | 0 | 0 | 0 | 20 | 3 | 2 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 |
128.60 | 27-262-14-CC,0 | 100 | 0 | 0 | Pleistocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 30 | 0 | 2 | 0 | 0 | 10 | 15 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
128.60 | 27-262-14-CC,0 | 100 | 0 | 0 | Pleistocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 80 | 0 | 0 | 0 | 0 | 50 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
129.38 | 27-262-15-1,75 | 20 | 70 | 10 | Pleistocene | RAD BEARING DETRITAL FORAM RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 44 | 25 | 0 | 0 | 0 | 0 | 10 | 1 | 2 | 1 | 0 | 0 | 5 | 0 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
130.88 | 27-262-15-2,75 | 0 | 70 | 30 | Pleistocene | CLAY BEARING RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 5 | 2 | 69 | 2 | 0 | 0 | 0 | 0 | 15 | 2 | 0 | 1 | 0 | 0 | 2 | 2 | 0 | 0 | 5 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
132.38 | 27-262-15-3,75 | 0 | 70 | 30 | Pleistocene | CLAY BEARING RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 5 | 2 | 69 | 2 | 0 | 0 | 0 | 0 | 15 | 2 | 0 | 1 | 0 | 0 | 2 | 2 | 0 | 0 | 5 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
133.88 | 27-262-15-4,75 | 0 | 70 | 30 | Pleistocene | CLAY BEARING RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 5 | 2 | 69 | 2 | 0 | 0 | 0 | 0 | 15 | 2 | 0 | 1 | 0 | 0 | 2 | 2 | 0 | 0 | 5 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
135.33 | 27-262-15-5,70 | 0 | 70 | 30 | Pleistocene | CLAY BEARING RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 5 | 2 | 69 | 2 | 0 | 0 | 0 | 0 | 20 | 2 | 0 | 1 | 0 | 0 | 2 | 2 | 0 | 0 | 5 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
136.88 | 27-262-15-6,75 | 0 | 70 | 30 | Pleistocene | CLAY BEARING RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 5 | 2 | 69 | 2 | 0 | 0 | 0 | 0 | 15 | 1 | 0 | 1 | 0 | 0 | 2 | 2 | 0 | 0 | 5 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
137.73 | 27-262-15-CC,0 | 0 | 0 | 0 | Pleistocene | FORAM BEARING RAD NANNO RICH CLAY | Dominat lithology; numerical abundance | 0 | 1 | 20 | 5 | 1 | 0 | 2 | 0 | 10 | 2 | 2 | 1 | 0 | 0 | 3 | 0 | 0 | 0 | 30 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 |
137.73 | 27-262-15-CC,0 | 100 | 0 | 0 | Pleistocene | FORAM BEARING RAD NANNO RICH CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 15 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
137.73 | 27-262-15-CC,0 | 100 | 30 | 70 | Pleistocene | FORAM BEARING RAD NANNO RICH CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 80 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
139.20 | 27-262-16-11,120 | 0 | 50 | 50 | Pleistocene | FORAM CLAY BEARING RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 45 | 5 | 0 | 0 | 0 | 0 | 10 | 2 | 0 | 1 | 0 | 0 | 3 | 0 | 0 | 0 | 5 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 |
140.25 | 27-262-16-2,75 | 0 | 50 | 50 | Pleistocene | FORAM CLAY BEARING RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 45 | 5 | 0 | 0 | 0 | 0 | 10 | 2 | 0 | 1 | 0 | 0 | 3 | 0 | 0 | 0 | 5 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 |
141.75 | 27-262-16-3,75 | 0 | 20 | 80 | Pleistocene | DETRITAL FORAM RAD BEARING NANNO CLAY | Dominat lithology; relative abundance | 0 | 1 | 27 | 5 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 30 | 0 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 |
143.00 | 27-262-16-4,50 | 90 | 10 | 0 | Pleistocene | DETRITAL FORAM SAND | Minor lithology; relative abundance | 0 | 0 | 0 | 88 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
144.75 | 27-262-16-5,75 | 0 | 80 | 20 | Pleistocene | CLAY FORAM BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 70 | 5 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 1 | 0 | 0 | 5 | 0 | 2 | 0 | 2 | 0 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
146.25 | 27-262-16-6,75 | 0 | 30 | 70 | Pleistocene | CLAY BEARING RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 60 | 1 | 0 | 0 | 0 | 0 | 25 | 1 | 2 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 5 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
147.10 | 27-262-16-CC,0 | 100 | 0 | 0 | Pleistocene | Dominat lithology; relative abundance | 0 | 0 | 0 | 63 | 0 | 0 | 0 | 0 | 25 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
147.10 | 27-262-16-CC,0 | 100 | 0 | 0 | Pleistocene | SILTY CLAY | numerical abundance | 15 | 0 | 0 | 52 | 0 | 0 | 0 | 0 | 15 | 15 | 1 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
148.90 | 27-262-17-1,90 | 0 | 10 | 90 | Pleistocene | RAD RICH CLAY NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 35 | 1 | 0 | 0 | 0 | 0 | 20 | 1 | 2 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 35 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
150.50 | 27-262-17-21,100 | 0 | 60 | 40 | Pleistocene | FORAM BEARING RAD CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 46 | 5 | 0 | 0 | 2 | 0 | 15 | 1 | 0 | 1 | 0 | 0 | 1 | 2 | 0 | 0 | 25 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 |
151.90 | 27-262-17-3,90 | 0 | 60 | 40 | Pleistocene | FORAM BEARING RAD CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 46 | 5 | 0 | 0 | 2 | 0 | 15 | 1 | 0 | 1 | 0 | 0 | 1 | 2 | 0 | 0 | 25 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 |
153.40 | 27-262-17-4,90 | 0 | 15 | 85 | Pleistocene | RAD CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 51 | 1 | 0 | 0 | 0 | 0 | 15 | 2 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 25 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 |
154.60 | 27-262-17-5,60 | 0 | 5 | 95 | Pleistocene | RAD CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 51 | 1 | 0 | 0 | 0 | 0 | 15 | 2 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 5 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 |
156.25 | 27-262-17-6,75 | 0 | 15 | 85 | Pleistocene | RAD CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 51 | 1 | 0 | 0 | 0 | 0 | 15 | 2 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 25 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 |
157.10 | 27-262-17-CC,0 | 100 | 0 | 0 | Pleistocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 60 | 0 | 2 | 0 | 0 | 10 | 10 | 2 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
157.10 | 27-262-17-CC,0 | 100 | 0 | 0 | Pleistocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 87 | 0 | 0 | 0 | 0 | 20 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
157.85 | 27-262-18-1,75 | 0 | 10 | 90 | Pleistocene | RAD CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 57 | 1 | 0 | 0 | 0 | 0 | 15 | 2 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 20 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 |
159.35 | 27-262-18-2,75 | 0 | 10 | 90 | Pleistocene | CLAY RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 57 | 1 | 0 | 0 | 0 | 0 | 20 | 2 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 15 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 |
160.70 | 27-262-18-3,60 | 0 | 20 | 80 | Pleistocene | CLAY RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 57 | 3 | 0 | 0 | 0 | 0 | 20 | 2 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 5 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 |
163.85 | 27-262-18-5,75 | 0 | 20 | 80 | Pleistocene | CLAY BEARING RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 67 | 1 | 0 | 0 | 0 | 0 | 2 | 2 | 2 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 10 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 |
165.05 | 27-262-18-6,45 | 0 | 30 | 70 | Pleistocene | RAD CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 45 | 2 | 0 | 0 | 0 | 0 | 15 | 2 | 2 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 20 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
166.20 | 27-262-18-CC,0 | 100 | 0 | 0 | Pleistocene | SILTY CLAY | Dominat lithology; relative abundance | 10 | 0 | 0 | 65 | 0 | 1 | 0 | 0 | 2 | 5 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
166.20 | 27-262-18-CC,0 | 100 | 0 | 0 | Pleistocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
167.45 | 27-262-19-1,75 | 0 | 30 | 70 | Pleistocene | RAD CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 45 | 2 | 0 | 0 | 0 | 0 | 15 | 2 | 2 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 20 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
168.95 | 27-262-19-2,75 | 0 | 0 | 0 | Pleistocene | RAD CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 45 | 2 | 0 | 0 | 0 | 0 | 20 | 1 | 0 | 2 | 0 | 0 | 2 | 0 | 2 | 0 | 20 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
170.45 | 27-262-19-3,75 | 0 | 0 | 0 | Pleistocene | RAD AND CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 45 | 2 | 0 | 0 | 0 | 0 | 20 | 1 | 0 | 2 | 0 | 0 | 2 | 0 | 2 | 0 | 20 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
171.95 | 27-262-19-4,75 | 1 | 60 | 39 | Pleistocene | CLAY RAD BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 54 | 2 | 0 | 0 | 0 | 0 | 15 | 1 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 |
173.45 | 27-262-19-5,75 | 1 | 60 | 39 | Pleistocene | CLAY RAD BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 54 | 2 | 0 | 0 | 0 | 0 | 15 | 1 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 |
174.95 | 27-262-19-6,75 | 1 | 60 | 39 | Pleistocene | CLAY RAD BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 54 | 2 | 0 | 0 | 0 | 0 | 15 | 1 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 |
175.80 | 27-262-19-CC,0 | 100 | 0 | 0 | Pleistocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 15 | 10 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
177.24 | 27-262-20-1,70 | 0 | 90 | 10 | Pleistocene | FORAM AND CLAY BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 57 | 4 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 10 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 |
178.79 | 27-262-20-2,75 | 0 | 90 | 10 | Pleistocene | FORAM AND CLAY BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 57 | 4 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 10 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 |
180.29 | 27-262-20-3,75 | 0 | 90 | 10 | Pleistocene | FORAM AND CLAY BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 57 | 4 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 10 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 |
181.79 | 27-262-20-4,75 | 0 | 90 | 10 | Pleistocene | RAD FORAM CLAY BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 61 | 4 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 10 | 0 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 |
183.29 | 27-262-20-5,75 | 0 | 90 | 10 | Pleistocene | FORAM AND CLAY BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 57 | 4 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 10 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 |
183.30 | 27-262-20-5,76 | 0 | 90 | 10 | Pleistocene | RAD FORAM CLAY BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 61 | 4 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 10 | 0 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 |
184.79 | 27-262-20-6,75 | 0 | 0 | 0 | Pleistocene | FORAM RAD BEARING CLAY NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 47 | 2 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 40 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 |
185.64 | 27-262-20-CC,0 | 100 | 0 | 0 | Pleistocene | SHELLY SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 2 | 2 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
185.64 | 27-262-20-CC,0 | 100 | 0 | 0 | Pleistocene | SHELLY SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 58 | 35 | 2 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
186.77 | 27-262-21-1,75 | 5 | 20 | 75 | Pleistocene | FORAM BEARING RAD RICH NANNO CLAY | Dominat lithology; relative abundance | 5 | 2 | 32 | 5 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 40 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
188.27 | 27-262-21-2,75 | 5 | 15 | 80 | Pleistocene | RAD AND CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 5 | 2 | 50 | 2 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 25 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
189.77 | 27-262-21-3,75 | 5 | 15 | 80 | Pleistocene | RAD AND CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 5 | 2 | 50 | 2 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 25 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
191.27 | 27-262-21-4,75 | 5 | 15 | 80 | Pleistocene | CLAY BEARING RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 5 | 2 | 65 | 2 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
192.77 | 27-262-21-5,75 | 5 | 15 | 80 | Pleistocene | DIATOM CLAY BEARING RAD RICH NANNO OOZE | Dominat lithology; relative abundance | 5 | 2 | 60 | 2 | 0 | 0 | 0 | 0 | 15 | 5 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
194.27 | 27-262-21-6,75 | 5 | 15 | 80 | Pleistocene | RAD BEARING CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 68 | 2 | 0 | 0 | 0 | 0 | 10 | 2 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 20 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
195.12 | 27-262-21-CC,0 | 100 | 0 | 0 | Pleistocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 95 | 2 | 2 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
197.25 | 27-262-22-2,75 | 0 | 30 | 70 | Pleistocene | RAD BEARING NANNO CLAY | Dominat lithology; relative abundance | 0 | 1 | 34 | 3 | 0 | 0 | 0 | 0 | 7 | 2 | 2 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 40 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
200.25 | 27-262-22-4,75 | 0 | 30 | 70 | Pleistocene | DIATOM RAD BEARING CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 10 | 1 | 0 | 3 | 0 | 0 | 0 | 0 | 7 | 4 | 2 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 20 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
201.75 | 27-262-22-5,75 | 0 | 30 | 70 | Pleistocene | RAD BEARING CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 62 | 3 | 0 | 0 | 0 | 0 | 5 | 2 | 2 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 15 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
202.60 | 27-262-22-CC,0 | 100 | 0 | 0 | Pleistocene | CALCAREOUS SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 65 | 0 | 2 | 0 | 0 | 1 | 4 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
202.60 | 27-262-22-CC,0 | 100 | 0 | 0 | Pleistocene | CALCAREOUS SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 97 | 0 | 2 | 0 | 0 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
205.25 | 27-262-23-1,75 | 0 | 0 | 0 | Pleistocene | CLAY BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 82 | 2 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
206.75 | 27-262-23-2,75 | 0 | 15 | 85 | Pleistocene | CLAY NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 57 | 2 | 0 | 0 | 0 | 0 | 3 | 1 | 2 | 1 | 0 | 0 | 2 | 0 | 0 | 2 | 30 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 |
208.25 | 27-262-23-3,75 | 0 | 15 | 85 | Pleistocene | CLAY NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 57 | 2 | 0 | 0 | 0 | 0 | 3 | 1 | 2 | 1 | 0 | 0 | 2 | 0 | 0 | 2 | 30 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 |
209.75 | 27-262-23-4,75 | 0 | 15 | 85 | Pleistocene | FORAM BEARING CLAY NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 54 | 5 | 0 | 0 | 0 | 0 | 3 | 1 | 2 | 1 | 0 | 0 | 2 | 0 | 0 | 2 | 30 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 |
211.25 | 27-262-23-5,75 | 0 | 15 | 85 | Pleistocene | FORAM BEARING CLAY NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 54 | 5 | 0 | 0 | 0 | 0 | 3 | 1 | 2 | 1 | 0 | 0 | 2 | 0 | 0 | 2 | 30 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 |
212.75 | 27-262-23-6,75 | 0 | 15 | 85 | Pleistocene | CLAY NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 57 | 2 | 0 | 0 | 0 | 0 | 3 | 1 | 2 | 1 | 0 | 0 | 2 | 0 | 0 | 2 | 30 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 |
213.60 | 27-262-23-CC,0 | 100 | 0 | 0 | Pleistocene | CALCAREOUS SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 85 | 2 | 0 | 0 | 0 | 10 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
213.60 | 27-262-23-CC,0 | 100 | 0 | 0 | Pleistocene | CALCAREOUS SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
214.75 | 27-262-24-1,75 | 0 | 0 | 0 | Pleistocene | 15 85 D CLAY NANNO OOZE | relative abundance | 0 | 1 | 57 | 2 | 0 | 0 | 0 | 0 | 3 | 1 | 2 | 1 | 0 | 0 | 2 | 0 | 0 | 2 | 30 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 |
216.25 | 27-262-24-2,75 | 0 | 15 | 85 | Pleistocene | CLAY NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 57 | 2 | 0 | 0 | 0 | 0 | 3 | 1 | 2 | 1 | 0 | 0 | 2 | 0 | 0 | 2 | 30 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 |
217.75 | 27-262-24-3,75 | 0 | 0 | 0 | Pleistocene | CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 1 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
219.25 | 27-262-24-4,75 | 0 | 0 | 0 | Pleistocene | CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 1 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
220.75 | 27-262-24-5,75 | 0 | 0 | 0 | Pleistocene | CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 73 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
221.20 | 27-262-24-51,120 | 0 | 0 | 0 | Pleistocene | CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 73 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
223.10 | 27-262-24-CC,0 | 100 | 0 | 0 | Pleistocene | SHELLY CALCAREOUS SILTY SAND | Dominat lithology; relative abundance | 0 | 0 | 0 | 90 | 0 | 2 | 0 | 0 | 3 | 1 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
223.10 | 27-262-24-CC,0 | 100 | 0 | 0 | Pleistocene | SHELLY CALCAREOUS SILTY SAND | Dominat lithology; relative abundance | 0 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
224.25 | 27-262-25-1,75 | 0 | 0 | 0 | Pleistocene | CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 73 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
225.75 | 27-262-25-2,75 | 0 | 0 | 0 | Pleistocene | CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 60 | 5 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
227.25 | 27-262-25-3,75 | 0 | 0 | 100 | Pleistocene | DIATOM BEARING CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 68 | 3 | 0 | 0 | 0 | 0 | 1 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
228.75 | 27-262-25-4,75 | 0 | 20 | 80 | Pleistocene | FORAM DIATOM BEARING CLAY RICH NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 68 | 4 | 0 | 0 | 0 | 0 | 1 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
230.25 | 27-262-25-5,75 | 0 | 20 | 80 | Pleistocene | RAD BEARING CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 5 | 2 | 70 | 5 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
231.10 | 27-262-25-CC,0 | 100 | 0 | 0 | Pleistocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 60 | 0 | 0 | 0 | 0 | 15 | 20 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
231.10 | 27-262-25-CC,0 | 100 | 0 | 0 | Pleistocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 85 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
234.30 | 27-262-26-1,75 | 0 | 20 | 80 | Pleistocene | RAD BEARING CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 5 | 2 | 70 | 5 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
235.80 | 27-262-26-2,75 | 0 | 20 | 80 | Pleistocene | FORAM CLAY BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 79 | 5 | 0 | 0 | 0 | 0 | 2 | 1 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
237.30 | 27-262-26-3,75 | 0 | 40 | 60 | Pleistocene | RAD FORAM CLAY BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 71 | 3 | 0 | 0 | 0 | 0 | 3 | 1 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
238.80 | 27-262-26-4,75 | 0 | 30 | 70 | Pleistocene | RAD FORAM BEARING CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 66 | 3 | 0 | 0 | 0 | 0 | 3 | 1 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 15 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
240.30 | 27-262-26-5,75 | 0 | 40 | 60 | Pleistocene | FORAM SPONGE CLAY BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 81 | 3 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 3 | 0 | 0 | 2 | 0 | 0 | 0 | 5 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
241.80 | 27-262-26-6,75 | 0 | 0 | 0 | Pleistocene | FORAM RAD BEARING CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 67 | 3 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 15 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
242.65 | 27-262-26-CC,0 | 100 | 0 | 0 | Pleistocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 85 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
243.07 | 27-262-27-1,0 | 0 | 0 | 0 | Pleistocene | FORAM RAD BEARING CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 67 | 3 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 15 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
245.64 | 27-262-27-21,107 | 0 | 0 | 0 | Pleistocene | RAD BEARING CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 62 | 5 | 0 | 0 | 0 | 0 | 3 | 2 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 20 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
246.82 | 27-262-27-3,75 | 0 | 0 | 0 | Pleistocene | RAD BEARING CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 62 | 5 | 0 | 0 | 0 | 0 | 3 | 2 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 20 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
249.82 | 27-262-27-5,75 | 0 | 0 | 0 | Pleistocene | FORAM BEARING CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 61 | 8 | 0 | 0 | 0 | 0 | 3 | 1 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
251.32 | 27-262-27-6,75 | 0 | 40 | 60 | Pleistocene | FORAM CLAY BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 76 | 5 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
252.17 | 27-262-27-CC,0 | 100 | 0 | 0 | Pleistocene | CALCAREOUS SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 85 | 0 | 0 | 2 | 0 | 2 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
252.17 | 27-262-27-CC,0 | 100 | 0 | 0 | Pleistocene | CALCAREOUS SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 94 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
252.75 | 27-262-28-1,75 | 50 | 25 | 25 | Pleistocene | CLAY RICH DETRITAL FORAM NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 47 | 20 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
254.25 | 27-262-28-2,75 | 0 | 40 | 60 | Pleistocene | FORAM CLAY BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 71 | 10 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 15 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
254.80 | 27-262-28-21,130 | 50 | 25 | 25 | Pleistocene | CLAY RICH DETRITAL FORAM NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 47 | 2 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
254.90 | 27-262-28-21,140 | 0 | 40 | 60 | Pleistocene | FORAM CLAY BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 71 | 10 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 15 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
255.75 | 27-262-28-3,75 | 40 | 10 | 50 | Pleistocene | CLAY DETRITAL FORAM RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 41 | 25 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
256.60 | 27-262-28-CC,0 | 100 | 0 | 0 | Pleistocene | SILTY CALCAREOUS CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 95 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
256.60 | 27-262-28-CC,0 | 100 | 0 | 0 | Pleistocene | SILTY CLACAREOUS CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 96 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
262.75 | 27-262-29-1,75 | 40 | 20 | 40 | Pleistocene | SPONGE BEARING CLAY DETRITAL FORAM RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 39 | 25 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
264.25 | 27-262-29-2,75 | 40 | 20 | 40 | Pleistocene | DETRITAL FORAM BEARING CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 66 | 10 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
264.46 | 27-262-29-2,96 | 0 | 0 | 0 | Pleistocene | VOLCANIC ASH | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | 0 |
265.67 | 27-262-29-3,67 | 20 | 80 | 0 | Pleistocene | VOLCANIC ASH | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | 0 |
265.75 | 27-262-29-3,75 | 0 | 0 | 0 | Pleistocene | FORAM BEARING CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 50 | 5 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 4 | 0 | 0 | 0 | 0 | 2 | 0 | 20 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 15 | 0 |
267.25 | 27-262-29-4,75 | 20 | 40 | 40 | Pleistocene | FORAM CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 60 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 18 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 10 | 0 |
268.75 | 27-262-29-5,75 | 30 | 20 | 50 | Pleistocene | CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 70 | 8 | 0 | 0 | 0 | 0 | 1 | 0 | 2 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 14 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
270.25 | 27-262-29-6,75 | 25 | 35 | 40 | Pleistocene | CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 70 | 8 | 0 | 0 | 0 | 0 | 2 | 2 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 11 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
271.10 | 27-262-29-CC,0 | 100 | 0 | 0 | Pleistocene | CALCAREOUS SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 95 | 2 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
271.10 | 27-262-29-CC,0 | 100 | 0 | 0 | Pleistocene | CALCAREOUS SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 96 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
271.75 | 27-262-30-1,75 | 40 | 20 | 40 | Pleistocene | CLAY FORAM RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 70 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 11 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 0 |
273.25 | 27-262-30-2,75 | 30 | 20 | 50 | Pleistocene | FORAM CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 72 | 12 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 15 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
274.75 | 27-262-30-3,75 | 35 | 20 | 45 | Pleistocene | FORAM CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 57 | 15 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 8 | 0 |
276.25 | 27-262-30-4,75 | 20 | 30 | 50 | Pleistocene | CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 70 | 8 | 0 | 0 | 0 | 2 | 1 | 8 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 20 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
277.75 | 27-262-30-5,75 | 35 | 15 | 50 | Pleistocene | FORAM CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 68 | 10 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 4 | 0 | 0 | 2 | 0 | 0 | 0 | 15 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
278.60 | 27-262-30-CC,0 | 100 | 0 | 0 | Pleistocene | CALCAREOUS SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 95 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
278.60 | 27-262-30-CC,0 | 100 | 0 | 0 | Pleistocene | CALCAREOUS SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 98 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
282.75 | 27-262-31-2,75 | 15 | 30 | 55 | Pleistocene | V.SLIGHTLY SANDY SILTY CALCAREOUS CLAY | Dominat lithology; relative abundance | 0 | 0 | 66 | 5 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 15 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 12 | 0 |
284.25 | 27-262-31-3,75 | 30 | 35 | 35 | Pleistocene | FORAM CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 56 | 12 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 |
285.75 | 27-262-31-4,75 | 30 | 30 | 40 | Pleistocene | FORAM CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 59 | 12 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 15 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 12 | 0 |
287.25 | 27-262-31-5,75 | 20 | 40 | 40 | Pleistocene | CLAY CARB RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 67 | 5 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 |
288.75 | 27-262-31-6,75 | 15 | 35 | 50 | Pleistocene | CLAY CARB RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 60 | 5 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 15 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 |
289.60 | 27-262-31-CC,0 | 100 | 0 | 0 | Pleistocene | CALCAREOUS SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 96 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
289.60 | 27-262-31-CC,0 | 100 | 0 | 0 | Pleistocene | CALCAREOUS SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 98 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
291.25 | 27-262-32-1,75 | 30 | 30 | 60 | Pleistocene | CLAY FORAM RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 69 | 10 | 0 | 0 | 0 | 2 | 2 | 0 | 2 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
292.75 | 27-262-32-2,75 | 15 | 40 | 45 | Pleistocene | CLAY CARB RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 74 | 5 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
294.25 | 27-262-32-3,75 | 15 | 40 | 45 | Pleistocene | CLAY CARB RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 74 | 5 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
295.75 | 27-262-32-4,75 | 10 | 60 | 30 | Pleistocene | CLAY CARB RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 64 | 5 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 |
297.25 | 27-262-32-5,75 | 10 | 45 | 45 | Pleistocene | CLAY CARB RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 76 | 3 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
298.75 | 27-262-32-6,75 | 25 | 35 | 40 | Pleistocene | CLAY CARB RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 0 | 8 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 12 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
299.60 | 27-262-32-CC,0 | 100 | 0 | 0 | Pleistocene | CALCAREOUS SILT CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 100 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
299.60 | 27-262-32-CC,0 | 100 | 0 | 0 | Pleistocene | CALCAREOUS SILT CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 98 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
300.25 | 27-262-33-1,75 | 15 | 55 | 30 | Pleistocene | CLAY CARB RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 67 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 12 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 |
301.75 | 27-262-33-2,75 | 20 | 30 | 50 | Pleistocene | CLAY CARB RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 66 | 8 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 12 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
303.25 | 27-262-33-3,75 | 30 | 30 | 40 | Pleistocene | CLAY CARB RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 73 | 8 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 0 |
304.35 | 27-262-33-4,35 | 0 | 0 | 0 | Pleistocene | VOLCANIC ASH | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
304.75 | 27-262-33-4,75 | 30 | 35 | 35 | Pleistocene | CLAY CARB FORAM RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 65 | 10 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 2 | 2 | 0 | 0 | 12 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 12 | 0 |
306.25 | 27-262-33-5,75 | 20 | 20 | 60 | Pleistocene | CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 76 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 12 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
308.60 | 27-262-33-CC,0 | 100 | 0 | 0 | Pleistocene | CALCAREOUS SILT CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 100 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
309.75 | 27-262-34-1,75 | 20 | 40 | 40 | Pleistocene | FORAM BEARING CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 55 | 10 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 15 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 |
311.25 | 27-262-34-2,75 | 0 | 0 | 0 | Pleistocene | CLAY MICARB RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 66 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 |
312.75 | 27-262-34-3,75 | 40 | 10 | 50 | Pleistocene | FORAM CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 56 | 15 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
314.25 | 27-262-34-4,75 | 20 | 20 | 60 | Pleistocene | FORAM CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 54 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 15 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 15 | 0 |
315.10 | 27-262-34-CC,0 | 100 | 0 | 0 | Pleistocene | CALCAREOUS SILT CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 100 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
315.10 | 27-262-34-CC,0 | 100 | 0 | 0 | Pleistocene | CALCAREOUS SILT CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 98 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
319.25 | 27-262-35-1,75 | 10 | 30 | 60 | Pleistocene | FORAM BEARING CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 72 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
320.75 | 27-262-35-2,75 | 0 | 0 | 0 | Pleistocene | FORAM BEARING CLAY RICH NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
322.25 | 27-262-35-3,75 | 0 | 40 | 60 | Pleistocene | FORAM BEARING CLAY NANNO OOZE | Dominat lithology; relative abundance | 5 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 35 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
323.75 | 27-262-35-4,75 | 0 | 0 | 0 | Pleistocene | GLASS (ASH) | Minor lithology; numerical abundance | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 84 | 0 | 10 | 0 |
325.25 | 27-262-35-5,75 | 10 | 30 | 60 | Pleistocene | FORAM BEARING NANNO CLAY | Dominat lithology; relative abundance | 0 | 2 | 35 | 5 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 40 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 15 | 0 |
326.75 | 27-262-35-6,75 | 10 | 30 | 60 | Pleistocene | FORAM BEARING NANNO CLAY | Dominat lithology; relative abundance | 0 | 2 | 35 | 5 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 40 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 15 | 0 |
327.60 | 27-262-35-CC,0 | 100 | 0 | 0 | Pleistocene | CALCAREOUS SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 97 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
327.60 | 27-262-35-CC,0 | 100 | 0 | 0 | Pleistocene | CALCAREOUS SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 98 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
329.05 | 27-262-36-1,75 | 20 | 5 | 70 | Pleistocene | NANNO BEARING DETRITAL FORAM SANDY CLAY | Dominat lithology; numerical abundance | 5 | 1 | 8 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
330.55 | 27-262-36-2,75 | 30 | 20 | 50 | Pleistocene | NANNO RICH DETRITAL FORAM SAND SILT CLAY | Dominat lithology; relative abundance | 0 | 1 | 20 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 38 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 10 | 0 |
332.05 | 27-262-36-3,75 | 0 | 0 | 0 | Pleistocene | FORAM BEARING CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 65 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 15 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
333.55 | 27-262-36-4,75 | 0 | 0 | 0 | Pleistocene | FORAM CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 60 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 15 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
335.05 | 27-262-36-5,75 | 0 | 0 | 0 | Pleistocene | FORAM BEARING CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 65 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 15 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
336.60 | 27-262-36-6,80 | 0 | 0 | 0 | Pleistocene | FORAM BEARING CLAY RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 65 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 15 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
337.40 | 27-262-36-CC,0 | 100 | 0 | 0 | Pleistocene | CALCAREOUS SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 78 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 |
337.40 | 27-262-36-CC,0 | 100 | 0 | 0 | Pleistocene | CALCAREOUS SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 88 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 |
338.77 | 27-262-37-1,75 | 60 | 10 | 30 | Upper pliocene | DETRITAL FORAM CLAYEY SAND | Dominat lithology; relative abundance | 10 | 2 | 10 | 59 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 20 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
340.27 | 27-262-37-2,75 | 65 | 20 | 15 | Upper pliocene | NANNO BEARING CLAY RICH DETRITAL FORAM SILTY SAND | Dominat lithology; relative abundance | 0 | 2 | 3 | 65 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 3 | 0 | 0 | 0 | 10 | 2 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 15 | 0 |
341.77 | 27-262-37-3,75 | 65 | 20 | 15 | Upper pliocene | NANNO BEARING CLAY RICH DETRITAL FORAM SILTY SAND | Dominat lithology; relative abundance | 0 | 2 | 3 | 65 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 3 | 0 | 0 | 0 | 10 | 2 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 15 | 0 |
343.27 | 27-262-37-4,75 | 50 | 20 | 30 | Upper pliocene | CLAY+DETRITAL FORAM RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 61 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
344.77 | 27-262-37-5,75 | 50 | 20 | 30 | Upper pliocene | CLAY+DETRITAL FORAM RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 61 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
346.27 | 27-262-37-6,75 | 50 | 20 | 30 | Upper pliocene | CLAY NANNO RICH DETRITAL FORAM SILTY SAND | Dominat lithology; relative abundance | 0 | 1 | 26 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
347.12 | 27-262-37-CC,0 | 100 | 0 | 0 | Upper pliocene | CALCAREOUS SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 78 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 |
347.12 | 27-262-37-CC,0 | 100 | 0 | 0 | Upper pliocene | CALCAREOUS SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 98 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
347.75 | 27-262-38-1,75 | 50 | 20 | 30 | Upper pliocene | CLAY RICH DETRITAL FORAM NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 50 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 19 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
349.25 | 27-262-38-2,75 | 50 | 20 | 30 | Upper pliocene | CLAY NANNO RICH DETRITAL FORAM SILTY SAND | Dominat lithology; relative abundance | 0 | 1 | 26 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
350.75 | 27-262-38-3,75 | 50 | 20 | 30 | Upper pliocene | CLAY NANNO RICH DETRITAL FORAM SILTY SAND | Dominat lithology; relative abundance | 0 | 1 | 26 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
352.25 | 27-262-38-4,75 | 50 | 20 | 30 | Upper pliocene | CLAY NANNO RICH DETRITAL FORAM SILTY SAND | Dominat lithology; relative abundance | 0 | 1 | 26 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
353.75 | 27-262-38-5,75 | 50 | 20 | 30 | Upper pliocene | CLAY NANNO RICH DETRITAL FORAM SILTY SAND | Dominat lithology; relative abundance | 0 | 1 | 26 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
354.60 | 27-262-38-CC,0 | 100 | 0 | 0 | Upper pliocene | CLAYEY SILTY SAND | Dominat lithology; relative abundance | 30 | 2 | 0 | 100 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
354.60 | 27-262-38-CC,0 | 100 | 0 | 0 | Upper pliocene | CLAYEY SILTY SAND | Dominat lithology; relative abundance | 0 | 0 | 0 | 64 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
357.25 | 27-262-39-1,75 | 60 | 20 | 20 | Upper pliocene | CLAY RICH DETRITAL FORAM NANNO OOZE | Dominat lithology; relative abundance | 10 | 1 | 40 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
357.25 | 27-262-39-1,75 | 60 | 20 | 20 | Upper pliocene | CLAY RICH DETRITAL FORAM NANNO OOZE | Dominat lithology; relative abundance | 10 | 1 | 45 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 15 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
358.75 | 27-262-39-2,75 | 65 | 20 | 15 | Upper pliocene | CLAY NANNO RICH DETRITAL FORAM SILTY SAND | Dominat lithology; relative abundance | 0 | 1 | 10 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
360.25 | 27-262-39-3,75 | 75 | 15 | 10 | Upper pliocene | CLAY BEARING NANNO RICH DETRITAL FORAM SAND | Dominat lithology; relative abundance | 0 | 1 | 10 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 5 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
361.75 | 27-262-39-4,75 | 65 | 20 | 15 | Upper pliocene | CLAY NANNO RICH DETRITAL FORAM SILTY SAND | Dominat lithology; relative abundance | 0 | 1 | 10 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
363.25 | 27-262-39-5,75 | 65 | 20 | 15 | Upper pliocene | CLAY NANNO RICH DETRITAL FORAM SILTY SAND | Dominat lithology; relative abundance | 0 | 1 | 10 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
364.75 | 27-262-39-6,75 | 65 | 20 | 15 | Upper pliocene | CLAY NANNO RICH DETRITAL FORAM SILTY SAND | Dominat lithology; relative abundance | 0 | 1 | 10 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
365.60 | 27-262-39-CC,0 | 100 | 0 | 0 | Upper pliocene | SILTY CLAY | Dominat lithology; relative abundance | 30 | 0 | 0 | 60 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
365.60 | 27-262-39-CC,0 | 100 | 0 | 0 | Upper pliocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 98 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 7 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
366.75 | 27-262-40-1,75 | 75 | 15 | 10 | Upper pliocene | CLAY NANNO BEARING DETRITAL FORAM SAND | Dominat lithology; relative abundance | 0 | 2 | 10 | 76 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 5 | 2 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
368.25 | 27-262-40-2,75 | 75 | 15 | 10 | Upper pliocene | CLAY NANNO BEARING DETRITAL FORAM SAND | Dominat lithology; relative abundance | 0 | 2 | 10 | 76 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 5 | 2 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
369.75 | 27-262-40-3,75 | 40 | 20 | 40 | Upper pliocene | CLAY DETRITAL FORAM NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 31 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 25 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
371.25 | 27-262-40-4,75 | 10 | 80 | 10 | Upper pliocene | CLAY NANNO BEARING DETRITAL FORAM SILT | Dominat lithology; relative abundance | 0 | 0 | 3 | 83 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 5 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
372.75 | 27-262-40-5,75 | 20 | 50 | 30 | Upper pliocene | NANNO MICARB BEARING CLAY RICH DETRITALFORAM SANDY SILT | Dominat lithology; numerical abundance | 10 | 2 | 5 | 67 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
373.60 | 27-262-40-CC,0 | 100 | 0 | 0 | Upper pliocene | CALCAREOUS SILTY SAND | Dominat lithology; relative abundance | 30 | 10 | 0 | 55 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 |
373.60 | 27-262-40-CC,0 | 100 | 0 | 0 | Upper pliocene | CALCAREOUS SILTY SAND | Dominat lithology; relative abundance | 0 | 0 | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
377.75 | 27-262-41-2,75 | 75 | 15 | 10 | Pliocene | CLAY NANNO BEARING MICARB RICH DETRITAL FORAM SILTY SAND | Dominat lithology; relative abundance | 25 | 1 | 5 | 62 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 5 | 2 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
379.25 | 27-262-41-3,75 | 75 | 15 | 10 | Pliocene | CLAY NANNO BEARING MICARB RICH DETRITAL FORAM SILTY SAND | Dominat lithology; relative abundance | 25 | 1 | 5 | 57 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 10 | 2 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
380.75 | 27-262-41-4,75 | 75 | 15 | 10 | Pliocene | CLAY NANNO BEARING MICARB RICH DETRITAL FORAM SILTY SAND | Dominat lithology; relative abundance | 25 | 1 | 5 | 57 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 10 | 2 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
382.25 | 27-262-41-5,75 | 60 | 30 | 15 | Pliocene | CLAY MICARB BEARING DETRITAL FORAM NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 48 | 35 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
383.75 | 27-262-41-6,75 | 60 | 30 | 15 | Pliocene | CLAY MICARB BEARING DETRITAL FORAM NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 48 | 35 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
384.60 | 27-262-41-CC,0 | 100 | 0 | 0 | Pliocene | CALCAREOUS CLAYEY SAND | Dominat lithology; relative abundance | 30 | 0 | 0 | 58 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 |
384.60 | 27-262-41-CC,0 | 100 | 0 | 0 | Pliocene | CALCAREOUS CLAYEY SAND | Dominat lithology; relative abundance | 0 | 0 | 0 | 85 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
387.25 | 27-262-42-2,75 | 50 | 30 | 20 | Middle pliocene | CLAY BEARING MICARB RICH DETRITAL FORAM NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 36 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 3 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 |
388.75 | 27-262-42-3,75 | 40 | 40 | 20 | Middle pliocene | CLAY BEARING MICARB RICH DETRITAL FORAM SILTY SAND | Dominat lithology; relative abundance | 0 | 2 | 10 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 10 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 38 | 0 |
390.25 | 27-262-42-4,75 | 70 | 20 | 10 | Middle pliocene | CLAY NANNO BEARING MICARB RICH DETRITAL FORAM SILTY SAND | Dominat lithology; relative abundance | 30 | 2 | 10 | 53 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
391.75 | 27-262-42-5,75 | 50 | 40 | 10 | Middle pliocene | CLAY BEARING MICARB DETRITAL FORAM SILTY SAND | Dominat lithology; relative abundance | 0 | 1 | 5 | 57 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 5 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 |
392.60 | 27-262-42-CC,0 | 100 | 0 | 0 | Middle pliocene | CALCAREOUS SILTY SAND | Dominat lithology; numerical abundance | 30 | 0 | 0 | 65 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
392.60 | 27-262-42-CC,0 | 100 | 0 | 0 | Middle pliocene | CALCAREOUS SILTY SAND | Dominat lithology; relative abundance | 0 | 0 | 0 | 98 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
395.25 | 27-262-43-1,75 | 70 | 20 | 10 | Middle pliocene | CLAY NANNO BEARING MICARB RICH DETRITAL FORAM SILTY SAND | Dominat lithology; relative abundance | 30 | 2 | 10 | 53 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
396.75 | 27-262-43-2,75 | 75 | 20 | 5 | Middle pliocene | NANNO BEARING MICARB RICH DETRITAL FORAM SAND | Dominat lithology; relative abundance | 0 | 1 | 10 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 27 | 0 |
397.60 | 27-262-43-CC,0 | 100 | 0 | 0 | Middle pliocene | CALCAREOUS SILTY CLAYEY SAND | Dominat lithology; numerical abundance | 60 | 0 | 0 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 |
397.60 | 27-262-43-CC,0 | 100 | 0 | 0 | Middle pliocene | CALCAREOUS SILTY CLAYEY SAND | Dominat lithology; relative abundance | 0 | 0 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
406.25 | 27-262-44-2,75 | 75 | 20 | 5 | Middle pliocene | NANNO CLAY BEARING MICARB RICH DETRITAL FORAM SAND | Dominat lithology; relative abundance | 0 | 1 | 5 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 5 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 27 | 0 |
407.75 | 27-262-44-3,75 | 30 | 50 | 20 | Middle pliocene | CLAY BEARING FORAM MICARB RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 44 | 20 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 3 | 0 | 0 | 0 | 5 | 2 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 |
408.60 | 27-262-44-CC,0 | 100 | 0 | 0 | Middle pliocene | CLAY BEARING FORAM MICARB RICH NANNO OOZE | Dominat lithology; relative abundance | 20 | 10 | 44 | 20 | 1 | 1 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 5 | 2 | 0 | 1 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 |
408.60 | 27-262-44-CC,0 | 100 | 0 | 0 | Middle pliocene | CLAY BEARING FORAM MICARB RICH NANNO OOZE | Dominat lithology; relative abundance | 60 | 2 | 0 | 30 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
408.60 | 27-262-44-CC,0 | 30 | 50 | 20 | Middle pliocene | CLAY BEARING FORAM MICARB RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
413.90 | 27-262-45-1,40 | 20 | 60 | 20 | Pliocene | CLAY NANNO BEARING FORAM RICH MICARB OOZE | Dominat lithology; relative abundance | 0 | 1 | 5 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 63 | 0 |
414.44 | 27-262-45-1,93.5 | 30 | 50 | 20 | Pliocene | CLAY NANNO BEARING FORAM MICARB OOZE | Dominat lithology; relative abundance | 0 | 1 | 5 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 59 | 0 |
414.45 | 27-262-45-1,95 | 0 | 0 | 0 | Pliocene | FORAM BEARING DOLOMITE | Minor lithology; numerical abundance | 0 | 90 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
414.80 | 27-262-45-11,130 | 0 | 0 | 0 | Pliocene | CLAY FORAM BEARING DOLOMITE | Minor lithology; relative abundance | 0 | 85 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
415.75 | 27-262-45-2,75 | 0 | 0 | 0 | Pliocene | CLAY BEARING FORAM RICH DOLOMITE | Dominat lithology; relative abundance | 0 | 82 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
417.25 | 27-262-45-3,75 | 0 | 0 | 0 | Pliocene | CLAY BEARING FORAM RICH DOLOMITE | Dominat lithology; relative abundance | 0 | 82 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
418.75 | 27-262-45-4,75 | 0 | 0 | 0 | Pliocene | CLAY BEARING FORAM RICH? DOLOMITE | Dominat lithology; relative abundance | 0 | 71 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
420.25 | 27-262-45-5,75 | 0 | 0 | 0 | Pliocene | CLAY BEARING FORAMS? RICH DOLOMITE | Dominat lithology; relative abundance | 0 | 87 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 3 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
421.75 | 27-262-45-6,75 | 0 | 0 | 0 | Pliocene | CLAY BEARING FORAM? RICH DOLOMITE | Dominat lithology; relative abundance | 0 | 77 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
422.60 | 27-262-45-CC,0 | 100 | 0 | 0 | Pliocene | CALCAREOUS SILTY SAND | Dominat lithology; numerical abundance | 59 | 30 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 |
422.60 | 27-262-45-CC,0 | 100 | 0 | 0 | Pliocene | CALCAREOUS SILTY SAND | Dominat lithology; relative abundance | 0 | 0 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
423.10 | 27-262-46-CC,0 | 0 | 0 | 0 | Pliocene | CLAY+DOLOMITE BEARING ? FORAM RICH MICARB OOZE | Dominat lithology; relative abundance | 0 | 5 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 82 | 0 |
434.10 | 27-262-47-CC,0 | 100 | 0 | 0 | Pliocene | BIOCALCARENITE | Dominat lithology; relative abundance | 57 | 40 | 0 | 5 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
434.10 | 27-262-47-CC,0 | 100 | 0 | 0 | Pliocene | BIOCALCARENITE | Dominat lithology; relative abundance | 90 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |