Yeats, Robert S; Haq, Bilal U (2005): Smear slide analysis of Hole 63-467 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230900
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
Wolfart, R; Shibata, Tsugio; Poore, Richard Z; Pisciotto, Kenneth A; Verma, Surendra P; Niem, Alan; Leinen, Margaret W; Grechin, V I; Douglas, A G; Denham, C R; Crouch, James; Bukry, David; Barron, John A; Yeats, Robert S; Haq, Bilal U (1981): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, LXIII, 967 pp, https://doi.org/10.2973/dsdp.proc.63.1981
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 33.849500 * Longitude: -120.757800
Date/Time Start: 1978-10-10T00:00:00 * Date/Time End: 1978-10-10T00:00:00
Minimum DEPTH, sediment/rock: 0.12 m * Maximum DEPTH, sediment/rock: 1033.98 m
Event(s):
63-467 * Latitude: 33.849500 * Longitude: -120.757800 * Date/Time: 1978-10-10T00:00:00 * Elevation: -2128.0 m * Penetration: 1041.5 m * Recovery: 399.1 m * Location: North Pacific/GAP * Campaign: Leg63 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 100 cores; 946.5 m cored; 38 m drilled; 42.2 % 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 | Chalcedony | Chalcedony | % | Smear slide analysis | ||
14 | Chert | Chert | % | Smear slide analysis | fragments | |
15 | Siliceous microfossils | Silic foss | % | Smear slide analysis | ||
16 | Radiolarians | Rad | % | Smear slide analysis | ||
17 | Diatoms | Diatoms | % | Smear slide analysis | ||
18 | Silicoflagellates | Silicoflag | % | Smear slide analysis | ||
19 | Spiculae | Spiculae | % | Smear slide analysis | ||
20 | Monazite | Mnz | % | Smear slide analysis | ||
21 | Quartz | Qz | % | Smear slide analysis | ||
22 | Feldspar | Fsp | % | Smear slide analysis | ||
23 | Zeolite | Zeo | % | Smear slide analysis | ||
24 | Mica | Mica | % | Smear slide analysis | ||
25 | Clay minerals | Clay min | % | Smear slide analysis | ||
26 | Glauconite | Glt | % | Smear slide analysis | ||
27 | Opaque minerals | Opaque | % | Smear slide analysis | ||
28 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
29 | Iron | Fe | % | Smear slide analysis | ||
30 | Heavy minerals | HM | % | Smear slide analysis | ||
31 | Rutile | Rt | % | Smear slide analysis | ||
32 | Zircon | Zrn | % | Smear slide analysis | ||
33 | Tourmaline | Tur | % | Smear slide analysis | ||
34 | Apatite | Ap | % | Smear slide analysis | ||
35 | Staurolite | St | % | Smear slide analysis | ||
36 | Epidote | Ep | % | Smear slide analysis | ||
37 | Hornblende | Hbl | % | Smear slide analysis | ||
38 | Amphibole | Amp | % | Smear slide analysis | ||
39 | Glaucophane | Gln | % | Smear slide analysis | ||
40 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
41 | Fragments | Fragm | % | Smear slide analysis | calcareous material | |
42 | Pumice | Pumice | % | Smear slide analysis | ||
43 | Rock fragments | Rock fragm | % | Smear slide analysis | ||
44 | Organic matter | OM | % | Smear slide analysis | organic debris | |
45 | Minerals | Minerals | % | Smear slide analysis | isotropic minerals | |
46 | Terrigenous | Terr | % | Smear slide analysis | terrigeneous detritus |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
5803 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 Chalcedony [%] | 14 Chert [%] | 15 Silic foss [%] | 16 Rad [%] | 17 Diatoms [%] | 18 Silicoflag [%] | 19 Spiculae [%] | 20 Mnz [%] | 21 Qz [%] | 22 Fsp [%] | 23 Zeo [%] | 24 Mica [%] | 25 Clay min [%] | 26 Glt [%] | 27 Opaque [%] | 28 Py [%] | 29 Fe [%] | 30 HM [%] | 31 Rt [%] | 32 Zrn [%] | 33 Tur [%] | 34 Ap [%] | 35 St [%] | 36 Ep [%] | 37 Hbl [%] | 38 Amp [%] | 39 Gln [%] | 40 Volc glass [%] | 41 Fragm [%] | 42 Pumice [%] | 43 Rock fragm [%] | 44 OM [%] | 45 Minerals [%] | 46 Terr [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.12 | 63-467-1-CC,0 | 2 | 14 | 74 | Quaternary | SILTY CLAY | relative abundance | 0 | 0 | 5 | 5 | 0 | 0 | 0 | 2 | 5 | 0 | 1 | 0 | 3 | 1 | 0 | 2 | 70 | 2 | 0 | 2 | 7 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
6.80 | 63-467-2-1,80 | 2 | 28 | 70 | Quaternary | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 5 | 5 | 0 | 0 | 0 | 2 | 10 | 2 | 3 | 0 | 1 | 0 | 0 | 2 | 75 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
7.46 | 63-467-2-11,146 | 2 | 30 | 68 | Quaternary | SILICEOUS SILTY CLAY (DIAT SPONGES) | relative abundance | 0 | 0 | 3 | 2 | 0 | 0 | 0 | 2 | 10 | 3 | 5 | 0 | 4 | 2 | 0 | 1 | 65 | 0 | 2 | 2 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
8.53 | 63-467-2-21,103 | 0 | 0 | 0 | Quaternary | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
10.85 | 63-467-2-4,35 | 3 | 25 | 72 | Quaternary | SILICEOUS SILTY CLAY (DIATOMACEOUS) | Dominat lithology; relative abundance | 2 | 0 | 5 | 1 | 0 | 0 | 0 | 2 | 12 | 3 | 5 | 0 | 4 | 2 | 0 | 2 | 60 | 2 | 0 | 1 | 4 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 7 |
11.58 | 63-467-2-CC,0 | 2 | 23 | 75 | Quaternary | SILTY CLAY | relative abundance | 0 | 0 | 2 | 3 | 0 | 0 | 0 | 1 | 10 | 2 | 5 | 0 | 3 | 2 | 0 | 1 | 70 | 1 | 0 | 0 | 2 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
16.70 | 63-467-3-11,120 | 4 | 40 | 56 | Quaternary | DIATOMACEOUS SILTY CLAY | relative abundance | 0 | 0 | 4 | 3 | 0 | 0 | 0 | 4 | 25 | 2 | 4 | 0 | 6 | 3 | 0 | 1 | 40 | 0 | 0 | 1 | 3 | 3 | 0 | 0 | 2 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 62 |
17.95 | 63-467-3-2,95 | 0 | 0 | 0 | Quaternary | SPONGE SPICULITE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 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 |
21.62 | 63-467-3-5,12 | 10 | 30 | 60 | Quaternary | SILTY CLAY | relative abundance | 2 | 0 | 10 | 2 | 0 | 0 | 0 | 3 | 10 | 3 | 6 | 0 | 10 | 3 | 0 | 1 | 40 | 0 | 0 | 2 | 3 | 4 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 58 |
22.60 | 63-467-3-CC,0 | 5 | 30 | 65 | Quaternary | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 5 | 3 | 0 | 0 | 0 | 2 | 5 | 1 | 5 | 0 | 5 | 2 | 0 | 2 | 70 | 0 | 0 | 2 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 82 |
26.10 | 63-467-4-11,110 | 15 | 45 | 40 | Quaternary | NANNOFOSSIL CLAYEY SILT | Dominat lithology; relative abundance | 2 | 2 | 30 | 1 | 0 | 0 | 0 | 2 | 5 | 3 | 5 | 0 | 10 | 3 | 0 | 1 | 2 | 0 | 0 | 2 | 4 | 3 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
37.27 | 63-467-5-21,127 | 1 | 19 | 80 | Quaternary | NANNO SILTY CLAY | Dominat lithology; relative abundance | 3 | 0 | 35 | 5 | 0 | 0 | 0 | 2 | 3 | 2 | 5 | 0 | 5 | 2 | 0 | 2 | 40 | 0 | 0 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 46 |
41.95 | 63-467-5-51,145 | 0 | 10 | 90 | Quaternary | NANNO CLAY | relative abundance | 4 | 0 | 35 | 0 | 0 | 1 | 0 | 2 | 2 | 0 | 4 | 0 | 4 | 1 | 0 | 2 | 46 | 0 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
44.60 | 63-467-6-1,60 | 0 | 17 | 83 | Quaternary | FORAM NANNO CLAY | Dominat lithology; relative abundance | 0 | 0 | 30 | 25 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 4 | 2 | 0 | 2 | 34 | 0 | 0 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 43 |
56.83 | 63-467-7-3,33 | 0 | 20 | 80 | Quaternary | FORAMINIFERAL CLAY | Dominat lithology; relative abundance | 0 | 0 | 2 | 10 | 0 | 0 | 0 | 2 | 2 | 2 | 4 | 0 | 5 | 2 | 0 | 1 | 68 | 0 | 0 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 81 |
56.90 | 63-467-7-3,40 | 0 | 25 | 75 | Quaternary | NANNO FORAM CLAY | Dominat lithology; relative abundance | 0 | 0 | 10 | 12 | 0 | 0 | 0 | 2 | 2 | 2 | 3 | 0 | 5 | 2 | 0 | 2 | 62 | 1 | 0 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 70 |
68.80 | 63-467-8-41,130 | 10 | 10 | 80 | Quaternary | NANNO DIATOMACEOUS CLAY | relative abundance | 4 | 0 | 10 | 6 | 0 | 0 | 0 | 3 | 11 | 2 | 8 | 0 | 4 | 1 | 0 | 1 | 42 | 2 | 0 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 55 |
69.56 | 63-467-8-5,56 | 70 | 10 | 20 | Quaternary | FORAMS QUARTOSE SAND | relative abundance | 0 | 0 | 4 | 10 | 0 | 0 | 0 | 1 | 1 | 0 | 5 | 0 | 40 | 8 | 0 | 3 | 20 | 1 | 0 | 1 | 0 | 4 | 0 | 1 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 75 |
72.20 | 63-467-8-CC,0 | 10 | 20 | 80 | Quaternary | DIATOMACEOUS SILTY CLAY | Dominat lithology; relative abundance | 5 | 0 | 6 | 3 | 0 | 0 | 0 | 2 | 10 | 2 | 8 | 0 | 8 | 1 | 0 | 1 | 51 | 1 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 63 |
74.50 | 63-467-9-2,50 | 0 | 20 | 80 | Cenozoic | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 2 | 2 | 2 | 5 | 0 | 5 | 0 | 0 | 0 | 86 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 93 |
76.72 | 63-467-9-31,122 | 0 | 20 | 80 | Cenozoic | SILICEOUS SILTY CLAY | Minor lithology; relative abundance | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 6 | 0 | 6 | 0 | 2 | 0 | 0 | 0 | 80 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 83 |
84.00 | 63-467-10-2,50 | 0 | 20 | 80 | Upper pliocene | SILTY CLAY | Dominat lithology; relative abundance | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 2 | 5 | 2 | 6 | 0 | 5 | 0 | 0 | 0 | 80 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
98.30 | 63-467-11-5,80 | 0 | 20 | 80 | Upper pliocene | DIATOMACEOUS CLAY | Dominat lithology; relative abundance | 2 | 0 | 5 | 1 | 0 | 0 | 0 | 2 | 15 | 1 | 15 | 0 | 2 | 2 | 0 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
101.76 | 63-467-12-1,76 | 0 | 20 | 80 | Upper pliocene | CLAY | Dominat lithology; numerical abundance | 10 | 0 | 10 | 1 | 0 | 0 | 0 | 1 | 8 | 1 | 10 | 0 | 2 | 0 | 0 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
112.60 | 63-467-13-2,60 | 0 | 20 | 80 | Upper pliocene | CLAY | Dominat lithology; relative abundance | 8 | 0 | 8 | 3 | 0 | 0 | 0 | 2 | 7 | 1 | 8 | 0 | 2 | 2 | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
125.00 | 63-467-14-4,50 | 0 | 20 | 80 | Upper pliocene | CLAY | Dominat lithology; relative abundance | 5 | 0 | 5 | 2 | 0 | 0 | 0 | 2 | 3 | 0 | 5 | 0 | 1 | 0 | 0 | 0 | 80 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
128.13 | 63-467-14-6,63 | 35 | 10 | 55 | Upper pliocene | SANDY CLAY | Minor lithology; relative abundance | 0 | 0 | 10 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 | 10 | 5 | 0 | 0 | 50 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
128.40 | 63-467-14-6,90 | 50 | 10 | 40 | Upper pliocene | CLAYEY ASH | Minor lithology; relative abundance | 0 | 0 | 5 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 1 | 0 | 0 | 2 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 0 |
130.76 | 63-467-15-11,126 | 0 | 40 | 60 | Upper pliocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 10 | 5 | 0 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 5 | 2 | 0 | 0 | 75 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
141.10 | 63-467-16-2,60 | 0 | 30 | 70 | Upper pliocene | SILTY CLAY | Dominat lithology; relative abundance | 10 | 0 | 5 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 | 10 | 0 | 0 | 2 | 60 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
150.70 | 63-467-17-2,70 | 0 | 30 | 70 | Upper pliocene | SILTY CLAY | relative abundance | 10 | 0 | 10 | 5 | 0 | 0 | 0 | 2 | 2 | 2 | 8 | 0 | 10 | 3 | 0 | 2 | 50 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
162.30 | 63-467-18-31,130 | 0 | 25 | 75 | Upper pliocene | SILICEOUS SILTY CLAY | relative abundance | 10 | 0 | 10 | 2 | 0 | 0 | 0 | 2 | 10 | 2 | 2 | 0 | 3 | 2 | 0 | 2 | 50 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
171.60 | 63-467-19-31,110 | 0 | 15 | 85 | Upper pliocene | SILICEOUS CLAY | relative abundance | 10 | 0 | 10 | 2 | 0 | 0 | 0 | 2 | 15 | 2 | 10 | 0 | 3 | 1 | 0 | 0 | 50 | 2 | 0 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
180.50 | 63-467-20-3,50 | 0 | 20 | 80 | Upper pliocene | DIATOMACEOUS CLAY | relative abundance | 15 | 0 | 5 | 2 | 0 | 0 | 0 | 2 | 20 | 0 | 5 | 0 | 3 | 1 | 0 | 0 | 50 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
187.30 | 63-467-21-1,80 | 5 | 15 | 80 | Upper pliocene | DIATOMACEOUS CLAY | relative abundance | 0 | 0 | 5 | 2 | 0 | 0 | 0 | 2 | 25 | 2 | 5 | 0 | 3 | 1 | 0 | 0 | 58 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
188.31 | 63-467-21-2,31 | 75 | 20 | 5 | Upper pliocene | QUARTOSE-FELDSPAR SAND | relative abundance | 4 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 1 | 0 | 5 | 0 | 60 | 20 | 0 | 2 | 5 | 2 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 95 |
205.52 | 63-467-23-1,2 | 0 | 30 | 70 | Upper pliocene | relative abundance | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 30 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 30 | |
215.00 | 63-467-24-1,0 | 10 | 20 | 70 | Upper pliocene | ARGILLACEOUS LIMESTONE | numerical abundance | 10 | 0 | 0 | 8 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 3 | 1 | 0 | 20 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 30 |
226.89 | 63-467-25-2,89 | 0 | 5 | 95 | Upper pliocene | NANNO CLAY | relative abundance | 10 | 0 | 31 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 5 | 0 | 1 | 1 | 0 | 2 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
227.81 | 63-467-25-3,31 | 80 | 10 | 10 | Upper pliocene | FINE FORAMINIFEROUS QTZ-FEL SAND | relative abundance | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 2 | 0 | 0 | 5 | 0 | 35 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
231.31 | 63-467-25-5,81 | 0 | 10 | 90 | Upper pliocene | NANNO CLAY | relative abundance | 10 | 0 | 16 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 15 | 0 | 10 | 5 | 0 | 2 | 37 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
236.20 | 63-467-26-2,70 | 10 | 20 | 70 | Pliocene | NANNO CLAY | relative abundance | 3 | 0 | 19 | 4 | 0 | 0 | 0 | 2 | 2 | 0 | 5 | 0 | 5 | 5 | 2 | 2 | 51 | 2 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 63 |
243.65 | 63-467-27-1,15 | 5 | 10 | 85 | Lower pliocene | NANNO CLAY | relative abundance | 0 | 0 | 25 | 6 | 0 | 0 | 0 | 2 | 2 | 0 | 6 | 0 | 5 | 2 | 0 | 3 | 39 | 0 | 0 | 1 | 10 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 21 |
243.92 | 63-467-27-1,42 | 5 | 10 | 85 | Lower pliocene | NANNO CLAY | relative abundance | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 2 | 4 | 1 | 10 | 0 | 8 | 3 | 0 | 1 | 36 | 0 | 10 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 59 |
245.63 | 63-467-27-2,63 | 90 | 8 | 2 | Lower pliocene | QUARTOSE FELDSPATHIC SAND (LITH RICH) | numerical abundance | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 3 | 0 | 5 | 0 | 35 | 25 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 10 | 0 | 0 | 72 |
253.68 | 63-467-28-1,68 | 0 | 25 | 75 | Lower pliocene | NANNO SILTY CLAY | relative abundance | 0 | 0 | 20 | 4 | 0 | 0 | 0 | 2 | 8 | 2 | 8 | 0 | 10 | 2 | 2 | 1 | 0 | 0 | 0 | 4 | 0 | 51 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 64 |
264.70 | 63-467-29-2,70 | 2 | 8 | 90 | Lower pliocene | NANNO CLAY | relative abundance | 8 | 0 | 28 | 0 | 0 | 0 | 0 | 2 | 3 | 0 | 8 | 0 | 5 | 1 | 0 | 1 | 39 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 41 |
275.08 | 63-467-30-3,8 | 85 | 10 | 5 | Lower pliocene | FINE GRAIN QUARTOSE-FELDSPATHIC SAND | Dominat lithology; relative abundance | 0 | 0 | 6 | 6 | 0 | 0 | 0 | 0 | 3 | 0 | 10 | 2 | 36 | 20 | 0 | 2 | 5 | 0 | 0 | 3 | 0 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 76 |
275.26 | 63-467-30-3,26 | 6 | 11 | 84 | Lower pliocene | NANNO CLAY | Dominat lithology; relative abundance | 5 | 0 | 20 | 5 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 6 | 2 | 0 | 1 | 45 | 0 | 0 | 3 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
302.30 | 63-467-33-2,30 | 0 | 20 | 80 | Lower pliocene | NANNO SILTY CLAY | relative abundance | 3 | 0 | 20 | 3 | 0 | 0 | 0 | 0 | 2 | 2 | 5 | 0 | 10 | 5 | 0 | 2 | 50 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
312.27 | 63-467-34-2,77 | 90 | 10 | 0 | Lower pliocene | FINE GRAIN QUARTOSE FELDSPATHIC SAND | Minor lithology; relative abundance | 5 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 45 | 25 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 |
313.12 | 63-467-34-3,12 | 0 | 0 | 0 | Lower pliocene | NANNO CLAY CLAYEY NANNO OOZE | numerical abundance | 0 | 0 | 53 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 2 | 0 | 3 | 3 | 0 | 0 | 37 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
331.10 | 63-467-36-2,60 | 0 | 30 | 70 | Lower pliocene | NANNO SILTY CLAY | Dominat lithology; relative abundance | 4 | 0 | 42 | 2 | 0 | 0 | 0 | 2 | 2 | 0 | 6 | 0 | 10 | 6 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
369.50 | 63-467-40-21,100 | 0 | 40 | 60 | Lower pliocene | NANNO SILTY CLAYSTONE | Dominat lithology; relative abundance | 0 | 0 | 40 | 2 | 0 | 0 | 0 | 2 | 2 | 2 | 5 | 0 | 6 | 2 | 0 | 0 | 40 | 2 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
371.30 | 63-467-40-31,130 | 0 | 10 | 90 | Lower pliocene | CLAYEY CHALK | Dominat lithology; relative abundance | 0 | 0 | 70 | 2 | 0 | 0 | 0 | 2 | 0 | 2 | 5 | 0 | 3 | 1 | 0 | 0 | 20 | 2 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
371.55 | 63-467-40-4,5 | 10 | 15 | 75 | Lower pliocene | SANDY CHALK | Minor lithology; numerical abundance | 10 | 0 | 50 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 5 | 0 | 5 | 2 | 0 | 0 | 25 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
376.87 | 63-467-41-1,37 | 0 | 10 | 90 | Lower pliocene | NANNO CLAYSTONE | Dominat lithology; relative abundance | 5 | 0 | 27 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 8 | 0 | 7 | 3 | 0 | 0 | 45 | 0 | 0 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 |
378.88 | 63-467-41-2,88 | 0 | 15 | 85 | Lower pliocene | NANNO CLAYSTONE | Dominat lithology; relative abundance | 3 | 0 | 28 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 6 | 0 | 7 | 3 | 0 | 0 | 45 | 0 | 0 | 7 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 |
379.20 | 63-467-41-21,120 | 1 | 14 | 85 | Lower pliocene | NANNO CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 20 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 6 | 0 | 7 | 3 | 0 | 0 | 50 | 0 | 0 | 10 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
382.63 | 63-467-41-5,13 | 2 | 8 | 90 | Lower pliocene | NANNO CLAYSTONE | relative abundance | 1 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 4 | 0 | 3 | 1 | 0 | 2 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
388.82 | 63-467-42-21,132 | 0 | 15 | 85 | Lower pliocene | NANNO CLAY | Dominat lithology; relative abundance | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 2 | 2 | 1 | 4 | 0 | 10 | 4 | 0 | 2 | 50 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 67 |
392.24 | 63-467-42-5,24 | 0 | 5 | 95 | Lower pliocene | NANNO CLAY | relative abundance | 0 | 0 | 27 | 0 | 0 | 0 | 0 | 2 | 4 | 1 | 10 | 0 | 7 | 2 | 0 | 2 | 44 | 1 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 |
395.60 | 63-467-43-CC,0 | 5 | 10 | 85 | Lower pliocene | NANNO CLAYSTONE | relative abundance | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 5 | 3 | 0 | 2 | 50 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 59 |
408.50 | 63-467-44-3,50 | 0 | 20 | 80 | Lower pliocene | NANNO CLAYSTONE | relative abundance | 0 | 0 | 15 | 2 | 0 | 0 | 0 | 1 | 2 | 1 | 8 | 0 | 7 | 6 | 0 | 1 | 57 | 2 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 63 |
413.00 | 63-467-44-6,50 | 0 | 20 | 80 | Lower pliocene | NANNO CLAYSTONE | numerical abundance | 0 | 0 | 8 | 1 | 0 | 0 | 0 | 8 | 6 | 3 | 13 | 0 | 10 | 6 | 0 | 1 | 42 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 |
418.39 | 63-467-45-3,89 | 5 | 10 | 85 | Lower pliocene | DIATOMACEOUS CLAYSTONE (SILICEOUS) | relative abundance | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 2 | 25 | 2 | 12 | 0 | 3 | 2 | 0 | 1 | 46 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
422.54 | 63-467-45-6,54 | 5 | 15 | 80 | Lower pliocene | SILICEOUS CLAYSTONE (DIAT & SPICULES) | relative abundance | 0 | 0 | 3 | 2 | 0 | 0 | 0 | 2 | 15 | 0 | 12 | 0 | 5 | 3 | 0 | 1 | 58 | 0 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
434.22 | 63-467-47-1,72 | 0 | 12 | 88 | Upper miocene | CLAYSTONE | Dominat lithology; relative abundance | 0 | 0 | 8 | 0 | 0 | 0 | 0 | 1 | 2 | 2 | 2 | 0 | 9 | 2 | 0 | 0 | 75 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 86 |
445.02 | 63-467-48-2,52 | 5 | 25 | 70 | Upper miocene | SILTY CLAYSTONE | relative abundance | 4 | 0 | 5 | 0 | 0 | 0 | 0 | 2 | 6 | 2 | 8 | 0 | 10 | 5 | 0 | 1 | 56 | 2 | 0 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
453.13 | 63-467-49-1,63 | 5 | 20 | 75 | Upper miocene | SILICEOUS SILTY CLAYSTONE | relative abundance | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 1 | 6 | 1 | 10 | 0 | 8 | 5 | 0 | 1 | 60 | 2 | 0 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
453.13 | 63-467-49-1,63 | 3 | 25 | 75 | Upper miocene | SILICEOUS SILTY CLAY (SPICULES) | relative abundance | 4 | 1 | 6 | 0 | 0 | 0 | 0 | 0 | 8 | 2 | 10 | 0 | 6 | 4 | 0 | 2 | 54 | 0 | 0 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 68 |
462.17 | 63-467-50-1,17 | 1 | 9 | 90 | Upper miocene | SILICEOUS CLAYSTONE (DRILLING SLURRY) | Dominat lithology; relative abundance | 7 | 0 | 8 | 2 | 0 | 0 | 0 | 0 | 3 | 0 | 7 | 0 | 5 | 3 | 0 | 0 | 65 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
462.40 | 63-467-50-CC,9 | 0 | 10 | 90 | Upper miocene | SILICEOUS CLAY | relative abundance | 5 | 1 | 7 | 2 | 0 | 0 | 0 | 0 | 5 | 0 | 8 | 0 | 5 | 2 | 0 | 0 | 65 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
473.23 | 63-467-51-2,23 | 0 | 10 | 90 | Upper miocene | SILICEOUS CLAYSTONE | Dominat lithology; relative abundance | 3 | 0 | 5 | 2 | 0 | 0 | 0 | 2 | 6 | 0 | 9 | 0 | 5 | 3 | 0 | 0 | 67 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
503.60 | 63-467-54-3,60 | 0 | 25 | 75 | Upper miocene | SILTY CLAYSTONE | Dominat lithology; relative abundance | 5 | 0 | 6 | 1 | 0 | 0 | 0 | 2 | 1 | 0 | 8 | 0 | 0 | 1 | 0 | 0 | 70 | 1 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
510.20 | 63-467-55-1,70 | 0 | 25 | 75 | Upper miocene | CALCAREOUS SILTY CLAYSTONE | Dominat lithology; relative abundance | 15 | 0 | 10 | 2 | 0 | 0 | 0 | 0 | 1 | 0 | 5 | 0 | 3 | 2 | 0 | 0 | 60 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
532.75 | 63-467-57-31,125 | 0 | 0 | 0 | Upper miocene | CALCAREOUS SILTY CLAYSTONE | Dominat lithology; relative abundance | 10 | 0 | 22 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 5 | 1 | 0 | 0 | 60 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
540.08 | 63-467-58-2,58 | 2 | 18 | 80 | Upper miocene | CALCAREOUS CLAYSTONE | numerical abundance | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 5 | 3 | 0 | 1 | 61 | 0 | 0 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
540.73 | 63-467-58-21,123 | 5 | 20 | 75 | Upper miocene | CALCAREOUS CLAYSTONE | numerical abundance | 24 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 6 | 2 | 0 | 1 | 59 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
542.60 | 63-467-58-4,10 | 90 | 10 | 0 | Upper miocene | FINE GRAINED QTZ FELDSPATHIC SAND | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 3 | 0 | 3 | 0 | 1 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
547.97 | 63-467-59-1,47 | 1 | 9 | 90 | Upper miocene | CALCAREOUS CLAYSTONE | relative abundance | 30 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 5 | 3 | 0 | 1 | 57 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 |
557.25 | 63-467-60-1,25 | 3 | 12 | 85 | Upper miocene | CALCAREOUS CLAYSTONE | relative abundance | 30 | 0 | 8 | 1 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 3 | 2 | 0 | 2 | 55 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
567.30 | 63-467-61-1,80 | 2 | 20 | 78 | Upper miocene | CALCAREOUS CLAYSTONE | numerical abundance | 0 | 0 | 8 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 2 | 0 | 1 | 79 | 0 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
577.60 | 63-467-62-CC,0 | 2 | 8 | 90 | Upper miocene | CALCAREOUS CLAYSTONE | Dominat lithology; numerical abundance | 20 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 2 | 0 | 1 | 52 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 65 |
587.44 | 63-467-63-2,44 | 2 | 8 | 90 | Upper miocene | CALCAREOUS CLAYSTONE | numerical abundance | 20 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 2 | 0 | 1 | 62 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
596.19 | 63-467-64-11,119 | 2 | 8 | 90 | Upper miocene | CALCAREOUS CLAYSTONE | relative abundance | 15 | 0 | 11 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 5 | 2 | 0 | 1 | 60 | 2 | 0 | 1 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
596.44 | 63-467-64-11,144 | 2 | 8 | 90 | Upper miocene | CALCAREOUS CLAYSTONE | numerical abundance | 23 | 0 | 15 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 4 | 2 | 0 | 1 | 42 | 0 | 0 | 3 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
614.45 | 63-467-66-1,45 | 0 | 10 | 90 | Upper miocene | CALCAREOUS CLAYSTONE | Dominat lithology; numerical abundance | 20 | 0 | 4 | 2 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 4 | 2 | 0 | 1 | 53 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
623.90 | 63-467-67-1,40 | 0 | 10 | 90 | Upper miocene | CLAYEY LIMESTONE | Minor lithology; relative abundance | 50 | 0 | 3 | 2 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 3 | 2 | 0 | 2 | 40 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
624.57 | 63-467-67-11,107 | 0 | 10 | 90 | Upper miocene | CALCAREOUS CLAYSTONE | Dominat lithology; relative abundance | 25 | 0 | 2 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 2 | 0 | 2 | 65 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
680.75 | 63-467-73-1,25 | 50 | 20 | 30 | Upper miocene | FORAMINIFERAL CLAYEY SANDSTONE | relative abundance | 15 | 0 | 5 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 7 | 0 | 2 | 25 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
692.11 | 63-467-74-2,61 | 0 | 15 | 85 | Upper miocene | CLAYEY CALC CLAYSTONE | relative abundance | 30 | 0 | 5 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 60 | 2 | 0 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
692.87 | 63-467-74-CC,2 | 0 | 0 | 0 | Upper miocene | NANNO CLAYEY CHALK | relative abundance | 3 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 10 | 0 | 2 | 45 | 2 | 0 | 7 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 |
709.39 | 63-467-76-1,39 | 0 | 5 | 95 | Upper miocene | CLAYEY NANNO CHALK | relative abundance | 10 | 0 | 65 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 20 | 2 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
718.71 | 63-467-77-1,21 | 55 | 30 | 15 | Upper miocene | LITHIC LAPILLI TUFF | Dominat lithology; relative abundance | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 20 | 2 | 2 | 16 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 0 |
719.60 | 63-467-77-11,110 | 0 | 10 | 90 | Upper miocene | NANNO CLAYSTONE | Dominat lithology; relative abundance | 8 | 0 | 20 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 2 | 0 | 2 | 60 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
720.77 | 63-467-77-2,77 | 0 | 10 | 90 | Upper miocene | NANNO CLAYSTONE | Dominat lithology; relative abundance | 4 | 0 | 25 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 2 | 2 | 4 | 60 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
728.40 | 63-467-78-1,40 | 1 | 9 | 90 | Upper miocene | CLAYEY NANNO CHALK | relative abundance | 30 | 0 | 45 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 22 | 0 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
737.88 | 63-467-79-1,38 | 0 | 10 | 90 | Upper miocene | CLAYEY NANNO CHALK | relative abundance | 15 | 0 | 65 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 17 | 0 | 0 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
741.44 | 63-467-79-3,94 | 0 | 5 | 95 | Upper miocene | NANNO CLAYEY LIMESTONE | numerical abundance | 30 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 28 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 28 |
749.25 | 63-467-80-2,75 | 0 | 0 | 0 | Upper miocene | LITHIC LAPILLI TUFF = HAND SPECIMEN | 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 | 0 | 0 | 0 | 0 | 0 | 0 |
776.09 | 63-467-83-1,59 | 0 | 15 | 85 | Miocene | NANNO CLAYEY CHALK | numerical abundance | 35 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 50 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
776.90 | 63-467-83-11,140 | 0 | 0 | 0 | Miocene | ALTERED VOLCATIC TUFF (VITRIC) | relative abundance | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 10 | 2 | 0 | 65 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 |
779.03 | 63-467-83-3,53 | 2 | 45 | 53 | Miocene | CLAYEY TUFF | Dominat lithology; numerical abundance | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 3 | 0 | 0 | 45 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 45 | 0 | 0 | 0 | 0 | 0 | 0 |
780.96 | 63-467-83-4,96 | 0 | 20 | 80 | Miocene | CLAYEY NANNO CHALK | Dominat lithology; relative abundance | 55 | 0 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 20 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
786.66 | 63-467-84-2,16 | 0 | 10 | 90 | Miocene | CLAYEY NANNO CHALK | Dominat lithology; numerical abundance | 10 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 0 | 1 | 44 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
814.00 | 63-467-87-1,50 | 0 | 0 | 0 | Middle miocene | CLAYEY NANNO CHALK | Dominat lithology; relative abundance | 15 | 0 | 40 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 1 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
814.30 | 63-467-87-1,80 | 0 | 30 | 70 | Middle miocene | SILTY CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 10 | 2 | 2 | 70 | 1 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
815.55 | 63-467-87-2,55 | 0 | 0 | 0 | Middle miocene | CALCAREOUS (NANNO) CLAYSTONE | Dominat lithology; relative abundance | 4 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 3 | 0 | 2 | 70 | 2 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
815.58 | 63-467-87-2,58 | 0 | 0 | 0 | Middle miocene | CALCAREOUS (NANNO) CLAYSTONE | Dominat lithology; relative abundance | 10 | 0 | 20 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 2 | 0 | 2 | 60 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
824.48 | 63-467-88-11,148 | 0 | 0 | 0 | Middle miocene | ALTERED VOLCANIC ASH VITRIC TUFF | relative abundance | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 97 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
825.71 | 63-467-88-21,121 | 0 | 10 | 90 | Middle miocene | CALCAREOUS CLAYSTONE | relative abundance | 15 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | 2 | 70 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 79 |
826.95 | 63-467-88-3,95 | 0 | 0 | 0 | Middle miocene | CALCITE ALTERED FINE GRAINS | relative abundance | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 20 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
834.92 | 63-467-89-2,92 | 80 | 0 | 10 | Middle miocene | CARBONATE ALTERED FINE GRAINS | numerical abundance | 84 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
837.75 | 63-467-89-4,75 | 0 | 20 | 80 | Middle miocene | CALCAREOUS SILTY CLAYSTONE | relative abundance | 20 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 18 | 7 | 0 | 2 | 47 | 3 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 72 |
837.96 | 63-467-89-4,96 | 0 | 5 | 95 | Middle miocene | NANNO CLAYEY CHALK | numerical abundance | 46 | 0 | 15 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 35 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 56 |
856.40 | 63-467-91-4,40 | 0 | 0 | 100 | Middle miocene | CLAYEY NANNO CHALK OR LIMESTONE | relative abundance | 15 | 0 | 52 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 30 | 0 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
875.04 | 63-467-93-4,4 | 5 | 30 | 55 | Middle miocene | NANNO CLAYEY CHALK | relative abundance | 25 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 1 | 0 | 2 | 33 | 0 | 0 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 43 |
899.29 | 63-467-96-1,29 | 0 | 10 | 90 | Middle miocene | NANNO CLAYEY CHALK | relative abundance | 35 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | 0 | 30 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 35 |
901.36 | 63-467-96-2,86 | 5 | 1 | 94 | Middle miocene | CALCAREOUS CLAYSTONE | relative abundance | 20 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 2 | 0 | 2 | 60 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 70 |
902.93 | 63-467-96-3,93 | 50 | 15 | 35 | Middle miocene | CARBONATE CEMENTED GLAUCONITE | numerical abundance | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 1 | 0 | 0 | 20 | 30 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 |
910.25 | 63-467-97-2,25 | 1 | 4 | 95 | Middle miocene | CALCAREOUS CLAYSTONE | relative abundance | 30 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 60 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
927.80 | 63-467-99-1,30 | 0 | 10 | 90 | Middle miocene | CLAYEY NANNO CHALK | Dominat lithology; relative abundance | 20 | 0 | 30 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 3 | 2 | 0 | 2 | 40 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
939.54 | 63-467-100-21,104 | 10 | 60 | 30 | Middle miocene | CALCAREOUS SANDY SILT | Minor lithology; numerical abundance | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 5 | 0 | 1 | 40 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
965.98 | 63-467-103-1,48 | 0 | 25 | 75 | Middle miocene | SILTY CLAYSTONE | Dominat lithology; relative abundance | 2 | 7 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 5 | 0 | 2 | 75 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
995.57 | 63-467-106-2,7 | 0 | 37 | 63 | Middle miocene | SILTY CLAYSTONE | relative abundance | 6 | 0 | 6 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 18 | 5 | 0 | 2 | 56 | 1 | 0 | 2 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 83 |
1007.12 | 63-467-107-3,62 | 1 | 25 | 74 | Middle miocene | CALCAREOUS SILTY CLAYSTONE | numerical abundance | 11 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 5 | 0 | 1 | 70 | 0 | 0 | 1 | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
1013.29 | 63-467-108-1,29 | 0 | 25 | 75 | Middle miocene | CALC SILTY CLAYSTONE | relative abundance | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 6 | 0 | 1 | 70 | 2 | 0 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
1033.98 | 63-467-110-2,48 | 1 | 0 | 99 | Middle miocene | CLAYEY LIMESTONE | numerical abundance | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 28 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |