Laughton, Anthony S; Berggren, William A (2005): Smear slide analysis of Hole 12-119. PANGAEA, https://doi.org/10.1594/PANGAEA.230346
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
Whitmarsh, Robert B; van Hinte, Jan E; Ruffman, A; Perch-Nielsen, Katharina; Musich, L F; Franz, Ulrich; Davies, Thomas A; Benson, Richard N; Laughton, Anthony S; Berggren, William A (1972): Initial Reports of the Deep Sea Drilling Project 12. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XII, 1243 pp, https://doi.org/10.2973/dsdp.proc.12.1972
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 45.031700 * Longitude: -7.974800
Date/Time Start: 1970-08-02T00:00:00 * Date/Time End: 1970-08-02T00:00:00
Minimum DEPTH, sediment/rock: 11.80 m * Maximum DEPTH, sediment/rock: 706.60 m
Event(s):
12-119 * Latitude: 45.031700 * Longitude: -7.974800 * Date/Time: 1970-08-02T00:00:00 * Elevation: -4447.0 m * Penetration: 711 m * Recovery: 192.8 m * Location: North Atlantic/SEAMOUNT * Campaign: Leg12 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 40 cores; 368 m cored; 0 m drilled; 52.4 % 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 | Radiolarians | Rad | % | Smear slide analysis | ||
14 | Diatoms | Diatoms | % | Smear slide analysis | ||
15 | Spiculae | Spiculae | % | Smear slide analysis | ||
16 | Minerals, other | Min other | % | Smear slide analysis | ||
17 | Phosphorite | Phosph | % | Smear slide analysis | ||
18 | Quartz | Qz | % | Smear slide analysis | ||
19 | Feldspar | Fsp | % | Smear slide analysis | ||
20 | Zeolite | Zeo | % | Smear slide analysis | ||
21 | Mica | Mica | % | Smear slide analysis | ||
22 | Clay minerals | Clay min | % | Smear slide analysis | ||
23 | Glauconite | Glt | % | Smear slide analysis | ||
24 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
25 | Iron | Fe | % | Smear slide analysis | ||
26 | Limonite | Lm | % | Smear slide analysis | ||
27 | Heavy minerals | HM | % | Smear slide analysis | ||
28 | Zircon | Zrn | % | Smear slide analysis | ||
29 | Tourmaline | Tur | % | Smear slide analysis | ||
30 | Hornblende | Hbl | % | Smear slide analysis | ||
31 | Pyroxene | Pyrox | % | Smear slide analysis | ||
32 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
33 | Palagonite | Palagonite | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
3328 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 Rad [%] | 14 Diatoms [%] | 15 Spiculae [%] | 16 Min other [%] | 17 Phosph [%] | 18 Qz [%] | 19 Fsp [%] | 20 Zeo [%] | 21 Mica [%] | 22 Clay min [%] | 23 Glt [%] | 24 Py [%] | 25 Fe [%] | 26 Lm [%] | 27 HM [%] | 28 Zrn [%] | 29 Tur [%] | 30 Hbl [%] | 31 Pyrox [%] | 32 Volc glass [%] | 33 Palagonite [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
11.80 | 12-119-1-2,30 | 0 | 60 | 60 | Pleistocene | FORAM NANNO OOZE | Minor lithology; relative abundance | 6 | 0 | 55 | 0 | 0 | 0 | 23 | 6 | 0 | 6 | 0 | 23 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
12.50 | 12-119-1-21,100 | 35 | 60 | 60 | Pleistocene | SANDY SILT | Dominat lithology; relative abundance | 23 | 0 | 23 | 23 | 0 | 0 | 0 | 6 | 0 | 6 | 6 | 6 | 6 | 0 | 6 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
13.35 | 12-119-1-3,35 | 10 | 60 | 60 | Pleistocene | SILTY CLAY | Dominat lithology; relative abundance | 23 | 0 | 6 | 0 | 0 | 0 | 0 | 6 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
13.75 | 12-119-1-3,75 | 35 | 60 | 60 | Pleistocene | SANDY SILT | Dominat lithology; numerical abundance | 15 | 0 | 37 | 15 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 15 | 0 | 4 | 4 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 |
14.50 | 12-119-1-31,150 | 35 | 60 | 60 | Pleistocene | SLIGHTLY SANDY SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 55 | 23 | 0 | 0 | 0 | 6 | 0 | 6 | 0 | 0 | 6 | 0 | 6 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
51.30 | 12-119-2-11,130 | 35 | 60 | 60 | Pleistocene | SANDY SILTY CLAY | Dominat lithology; relative abundance | 6 | 0 | 55 | 23 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 23 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 |
51.70 | 12-119-2-2,20 | 35 | 60 | 35 | Pleistocene | SANDY SILT | Minor lithology; numerical abundance | 4 | 0 | 16 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 16 | 4 | 4 | 0 | 0 | 16 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 39 | 0 |
52.48 | 12-119-2-2,98 | 10 | 35 | 60 | Pleistocene | SILTY CLAY | Dominat lithology; numerical abundance | 4 | 0 | 52 | 16 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 16 | 4 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 |
53.90 | 12-119-2-3,90 | 0 | 35 | 60 | Pleistocene | SLIGHTLY SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 55 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 6 | 6 | 0 | 0 | 6 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
56.20 | 12-119-2-5,20 | 10 | 35 | 60 | Pleistocene | SILTY CLAY | Dominat lithology; relative abundance | 6 | 0 | 55 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 6 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
56.80 | 12-119-2-5,80 | 35 | 35 | 60 | Pleistocene | SLIGHTLY SANDY CLAY | Dominat lithology; relative abundance | 0 | 0 | 55 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 6 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
57.60 | 12-119-2-CC,0 | 0 | 35 | 85 | Pleistocene | SLIGHTLY SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 55 | 23 | 0 | 0 | 0 | 0 | 0 | 6 | 6 | 0 | 6 | 0 | 0 | 6 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
100.40 | 12-119-3-1,40 | 35 | 60 | 60 | Pliocene | SANDY SILT | Dominat lithology; relative abundance | 0 | 0 | 55 | 23 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 23 | 6 | 0 | 0 | 6 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 |
101.30 | 12-119-3-11,130 | 35 | 60 | 60 | Pliocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 55 | 23 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 23 | 6 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
102.25 | 12-119-3-2,75 | 10 | 60 | 60 | Pliocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 55 | 23 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 23 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
103.10 | 12-119-3-CC,0 | 0 | 35 | 60 | Pliocene | SLIGHTLY SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 55 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 6 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 6 |
150.75 | 12-119-4-1,75 | 0 | 60 | 60 | Upper miocene | SILTY CLAY | Dominat lithology; relative abundance | 6 | 0 | 75 | 6 | 0 | 0 | 0 | 6 | 0 | 6 | 6 | 23 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
152.30 | 12-119-4-2,80 | 10 | 35 | 60 | Upper miocene | SILTY CLAY | Dominat lithology; numerical abundance | 15 | 0 | 36 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 15 | 0 | 0 | 4 | 15 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 4 | 0 |
153.10 | 12-119-4-CC,0 | 0 | 10 | 60 | Upper miocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 55 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 6 | 6 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
201.75 | 12-119-5-3,75 | 0 | 35 | 85 | Middle miocene | SLIGHTLY SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 75 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 23 | 6 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
202.60 | 12-119-5-CC,0 | 0 | 10 | 60 | Middle miocene | CLAY | Dominat lithology; relative abundance | 23 | 0 | 55 | 6 | 0 | 0 | 6 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
241.30 | 12-119-6-11,130 | 0 | 60 | 60 | Lower miocene | SILTY CLAY | Dominat lithology; numerical abundance | 0 | 0 | 37 | 0 | 4 | 0 | 16 | 0 | 0 | 4 | 4 | 16 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 16 | 0 |
243.75 | 12-119-6-3,75 | 0 | 60 | 60 | Lower miocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 55 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
249.55 | 12-119-7-1,55 | 0 | 60 | 60 | Lower miocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 55 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 6 | 0 | 6 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
251.25 | 12-119-7-2,75 | 0 | 60 | 60 | Lower miocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 55 | 6 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
252.75 | 12-119-7-3,75 | 0 | 60 | 60 | Lower miocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 55 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 23 | 6 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
258.80 | 12-119-8-1,80 | 0 | 60 | 60 | Lower miocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 23 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 6 | 23 | 6 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 |
260.90 | 12-119-8-21,140 | 10 | 60 | 60 | Lower miocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 55 | 0 | 23 | 23 | 23 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
260.98 | 12-119-8-21,148 | 10 | 60 | 60 | Lower miocene | SILTY CLAY | Minor lithology; relative abundance | 0 | 0 | 55 | 0 | 6 | 6 | 23 | 0 | 0 | 0 | 6 | 0 | 6 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 6 | 0 |
261.75 | 12-119-8-3,75 | 0 | 60 | 60 | Lower miocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 55 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
262.10 | 12-119-8-31,110 | 35 | 60 | 60 | Lower miocene | SANDY SILT | Dominat lithology; numerical abundance | 0 | 0 | 14 | 0 | 0 | 0 | 33 | 0 | 0 | 0 | 0 | 14 | 3 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 33 | 0 |
262.80 | 12-119-8-4,30 | 0 | 60 | 60 | Lower miocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 55 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
263.50 | 12-119-8-41,100 | 35 | 60 | 60 | Lower miocene | SANDY SILT | Dominat lithology; numerical abundance | 0 | 0 | 11 | 0 | 0 | 11 | 11 | 3 | 0 | 0 | 3 | 11 | 3 | 0 | 3 | 5 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 36 | 0 |
264.40 | 12-119-8-5,40 | 35 | 60 | 60 | Lower miocene | SANDY SILT | Dominat lithology; numerical abundance | 0 | 0 | 3 | 0 | 12 | 0 | 12 | 0 | 0 | 0 | 0 | 12 | 12 | 0 | 0 | 12 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 39 | 0 |
269.00 | 12-119-9-2,50 | 10 | 60 | 60 | Lower miocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 55 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 6 | 23 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 |
269.50 | 12-119-9-21,100 | 0 | 60 | 60 | Lower miocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 55 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 23 | 6 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 6 |
276.98 | 12-119-10-1,70 | 0 | 60 | 60 | Lower miocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 55 | 0 | 6 | 0 | 23 | 0 | 0 | 0 | 0 | 15 | 6 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
278.28 | 12-119-10-2,50 | 35 | 60 | 60 | Lower miocene | SANDY SILT | Dominat lithology; relative abundance | 0 | 0 | 55 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 6 | 23 | 6 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
279.58 | 12-119-10-3,30 | 0 | 60 | 60 | Lower miocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 55 | 0 | 6 | 0 | 23 | 0 | 0 | 0 | 6 | 6 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 6 |
285.03 | 12-119-11-1,75 | 35 | 60 | 60 | Lower miocene | SLIGHTLY SANDY SILT | Dominat lithology; relative abundance | 0 | 0 | 55 | 0 | 6 | 0 | 6 | 0 | 0 | 0 | 0 | 6 | 6 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
295.25 | 12-119-12-2,75 | 0 | 60 | 60 | Oligocene | SILTY NANNO CLAY | Dominat lithology; relative abundance | 0 | 0 | 55 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 6 | 6 | 6 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
304.25 | 12-119-13-2,75 | 0 | 35 | 60 | Oligocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 55 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 6 | 6 | 0 | 0 | 6 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
313.25 | 12-119-14-2,75 | 0 | 35 | 60 | Upper oligocene | SLIGHTLY SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 6 | 0 | 0 | 6 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
323.75 | 12-119-15-3,75 | 0 | 60 | 60 | Upper oligocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 6 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
324.50 | 12-119-15-4,0 | 0 | 35 | 60 | Upper oligocene | CLAY | Dominat lithology; relative abundance | 6 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 6 | 75 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
324.50 | 12-119-15-4,0 | 0 | 35 | 85 | Upper oligocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
324.62 | 12-119-15-4,12 | 0 | 35 | 60 | Upper oligocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 6 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
325.20 | 12-119-15-4,70 | 0 | 35 | 60 | Upper oligocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 6 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
327.11 | 12-119-15-51,111 | 10 | 35 | 60 | Upper oligocene | SANDY SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 |
329.10 | 12-119-15-CC,0 | 0 | 85 | 10 | Upper oligocene | COCCOLITH OOZE | Dominat lithology; relative abundance | 6 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
331.25 | 12-119-16-2,75 | 0 | 35 | 60 | Upper oligocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 6 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
343.25 | 12-119-17-4,75 | 10 | 35 | 60 | Middle oligocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 6 |
345.60 | 12-119-17-CC,0 | 0 | 85 | 60 | Lower oligocene | NANNO MARL OOZE | Dominat lithology; numerical abundance | 13 | 0 | 43 | 0 | 0 | 0 | 3 | 0 | 0 | 13 | 0 | 0 | 6 | 0 | 0 | 3 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 13 | 0 |
354.00 | 12-119-18-5,75 | 0 | 35 | 60 | Lower oligocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
356.35 | 12-119-18-CC,0 | 0 | 85 | 10 | Middle eocene | COCCOLITH CHALK OOZE | Dominat lithology; relative abundance | 23 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
358.53 | 12-119-19-2,75 | 0 | 35 | 60 | Middle eocene | SILTY CLAY | Dominat lithology; relative abundance | 6 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 6 | 0 | 0 | 6 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
365.38 | 12-119-19-CC,0 | 0 | 60 | 85 | Middle eocene | SILTY NANNO CLAY | Dominat lithology; numerical abundance | 3 | 0 | 40 | 0 | 12 | 0 | 12 | 0 | 0 | 3 | 0 | 0 | 3 | 0 | 0 | 12 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 12 | 0 |
365.75 | 12-119-20-1,75 | 0 | 35 | 60 | Middle eocene | SILTY CLAY | Dominat lithology; relative abundance | 6 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 6 | 0 | 0 | 6 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
368.75 | 12-119-20-3,75 | 0 | 35 | 60 | Middle eocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 6 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
369.60 | 12-119-20-CC,0 | 0 | 60 | 60 | Middle eocene | NANNO MARL OOZE | Dominat lithology; relative abundance | 6 | 0 | 75 | 0 | 0 | 0 | 6 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 6 |
378.03 | 12-119-21-3,75 | 0 | 35 | 60 | Middle eocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 6 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
385.25 | 12-119-22-2,75 | 0 | 35 | 60 | Middle eocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 6 | 0 | 0 | 6 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
386.10 | 12-119-22-CC,0 | 0 | 60 | 85 | Middle eocene | NANNOFOSSIL MARL OOZE | Dominat lithology; relative abundance | 6 | 6 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 6 | 0 | 0 | 6 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 6 |
393.60 | 12-119-23-CC,0 | 0 | 60 | 60 | Lower eocene | NANNO MARL OOZE | Dominat lithology; numerical abundance | 3 | 12 | 28 | 0 | 0 | 0 | 0 | 0 | 0 | 12 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 12 | 0 | 0 | 0 | 0 | 3 | 28 | 3 |
410.10 | 12-119-24-CC,0 | 0 | 60 | 85 | Upper paleocene | SILTY NANNO CLAY | Dominat lithology; numerical abundance | 10 | 10 | 31 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 3 | 0 | 0 | 3 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 10 | 22 |
413.10 | 12-119-25-CC,0 | 0 | 85 | 35 | Upper paleocene | NANNO CHALK OOZE | Dominat lithology; numerical abundance | 36 | 0 | 48 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 4 |
419.70 | 12-119-26-1,70 | 0 | 85 | 60 | Upper paleocene | MARLY COCCOLITH CLAY | Dominat lithology; relative abundance | 23 | 0 | 75 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 6 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
420.10 | 12-119-26-11,110 | 0 | 35 | 85 | Upper paleocene | SILTY MARLY CLAY | Dominat lithology; numerical abundance | 27 | 0 | 37 | 3 | 0 | 0 | 0 | 0 | 0 | 12 | 0 | 0 | 3 | 0 | 0 | 12 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 3 | 0 |
428.75 | 12-119-27-1,75 | 0 | 60 | 35 | Upper paleocene | COCCOLITH MARL OOZE | Dominat lithology; relative abundance | 23 | 0 | 75 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
429.60 | 12-119-27-CC,0 | 0 | 35 | 85 | Upper paleocene | SILTY CLAY | Dominat lithology; relative abundance | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 75 | 0 | 6 | 6 | 0 | 0 | 6 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 12 | 23 |
445.25 | 12-119-28-2,75 | 0 | 85 | 35 | Upper paleocene | COCCOLITH OOZE | Dominat lithology; numerical abundance | 16 | 0 | 52 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 4 | 4 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 16 | 0 |
460.20 | 12-119-29-11,120 | 0 | 85 | 35 | Upper paleocene | RECRYSTALLIZED COCCOLITH OOZE | Dominat lithology; numerical abundance | 53 | 0 | 39 | 4 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
462.75 | 12-119-29-3,75 | 0 | 85 | 10 | Upper paleocene | RECRYSTALLIZED NANNO LIMESTONE | Dominat lithology; relative abundance | 75 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
464.30 | 12-119-29-4,80 | 0 | 85 | 35 | Upper paleocene | RECRYSTALLIZED COCCOLITH MARL | Dominat lithology; numerical abundance | 51 | 0 | 37 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 4 |
465.10 | 12-119-29-CC,0 | 0 | 85 | 10 | Upper paleocene | COCCOLITH CHALK OOZE | Dominat lithology; numerical abundance | 48 | 0 | 48 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
465.10 | 12-119-29-CC,0 | 0 | 85 | 10 | Upper paleocene | COCCOLITH CHALK OOZE | Dominat lithology; numerical abundance | 48 | 0 | 48 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
494.10 | 12-119-30-11,110 | 0 | 85 | 60 | Upper paleocene | RECRYSTALLIZED COCCOLITH MARL | Dominat lithology; relative abundance | 75 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
495.25 | 12-119-30-2,75 | 0 | 85 | 35 | Upper paleocene | RECRYSTALLIZED NANNO MARL | Dominat lithology; relative abundance | 75 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 23 |
498.25 | 12-119-30-4,75 | 0 | 85 | 35 | Upper paleocene | RECRYSTALLIZED COCCOLITH MARL | Dominat lithology; numerical abundance | 42 | 0 | 42 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 3 |
498.35 | 12-119-30-4,85 | 0 | 0 | 0 | Upper paleocene | RECRYSTALLIZED COCCOLITH MARL | Minor lithology; numerical abundance | 34 | 0 | 34 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 3 | 0 | 0 | 10 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 10 | 3 |
498.40 | 12-119-30-4,90 | 0 | 85 | 35 | Upper paleocene | RECRYSTALLIZED COCCOLITH MARL | Minor lithology; numerical abundance | 40 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 12 |
499.71 | 12-119-30-5,71 | 0 | 85 | 35 | Upper paleocene | RECRYSTALLIZED COCCOLITH MARL | Dominat lithology; relative abundance | 75 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
501.25 | 12-119-30-6,75 | 0 | 85 | 10 | Upper paleocene | RECRYSTALLIZED COCCOLITH MARL | Dominat lithology; relative abundance | 75 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 6 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
502.10 | 12-119-30-CC,0 | 0 | 85 | 35 | Upper paleocene | RECRYSTALLIZED CARBONATE SILT | Dominat lithology; relative abundance | 75 | 0 | 6 | 6 | 0 | 6 | 0 | 0 | 0 | 6 | 0 | 0 | 6 | 0 | 0 | 6 | 0 | 6 | 0 | 0 | 0 | 0 | 6 | 0 | 0 |
543.75 | 12-119-31-1,75 | 0 | 85 | 35 | Upper paleocene | RECRYSTALLIZED COCCOLITH MARL | Dominat lithology; relative abundance | 75 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 |
549.75 | 12-119-31-5,75 | 0 | 85 | 10 | Upper paleocene | COCCOLITH CHALK OOZE | Dominat lithology; numerical abundance | 37 | 0 | 45 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 |
549.75 | 12-119-31-5,75 | 10 | 85 | 35 | Upper paleocene | COCCOLITH CHALK OOZE | Dominat lithology; numerical abundance | 45 | 0 | 51 | 4 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
550.60 | 12-119-31-CC,0 | 0 | 85 | 35 | Upper paleocene | PURE NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
593.70 | 12-119-32-2,20 | 0 | 85 | 35 | Upper paleocene | RECRYSTALLIZED COCCOLITH MARL | Dominat lithology; relative abundance | 75 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
594.43 | 12-119-32-2,93 | 0 | 85 | 35 | Upper paleocene | RECRYSTALLIZED COCCOLITH MARL | Dominat lithology; relative abundance | 75 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
622.57 | 12-119-34-1,57 | 0 | 85 | 35 | Upper paleocene | RECRYSTALLIZED NANNO MARL | Dominat lithology; relative abundance | 75 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 6 |
623.60 | 12-119-34-CC,0 | 0 | 85 | 35 | Upper paleocene | RECRYSTALLIZED COCCOLITH MARL | Dominat lithology; relative abundance | 75 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
654.10 | 12-119-36-CC,0 | 0 | 35 | 10 | Upper paleocene | BRAARUDOSPHAERA MARL OOZE | Dominat lithology; numerical abundance | 48 | 0 | 48 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 |
667.15 | 12-119-37-4,65 | 0 | 85 | 60 | Upper paleocene | NANNO MARL | Dominat lithology; numerical abundance | 11 | 0 | 36 | 3 | 0 | 0 | 0 | 0 | 0 | 27 | 3 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 3 | 0 | 0 | 0 | 3 | 11 | 0 |
677.52 | 12-119-38-3,52 | 0 | 85 | 35 | Upper paleocene | NANNO MARL | Dominat lithology; numerical abundance | 42 | 0 | 42 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 3 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 |
678.25 | 12-119-38-31,125 | 0 | 85 | 35 | Upper paleocene | RECRYSTALLIZED COCCOLITH MARL | Dominat lithology; numerical abundance | 33 | 0 | 33 | 10 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
678.70 | 12-119-38-4,20 | 0 | 85 | 35 | Upper paleocene | RECRYSTALLIZED NANNO MARL | Dominat lithology; numerical abundance | 41 | 0 | 41 | 3 | 0 | 3 | 0 | 0 | 0 | 3 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 |
678.90 | 12-119-38-4,40 | 0 | 85 | 35 | Upper paleocene | RECRYSTALLIZED NANNO MARL | Dominat lithology; numerical abundance | 48 | 0 | 48 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 |
679.75 | 12-119-38-41,125 | 0 | 85 | 10 | Upper paleocene | RECRYSTALLIZED COCCOLITH OOZE | Dominat lithology; relative abundance | 75 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
680.10 | 12-119-38-CC,0 | 0 | 60 | 60 | Upper paleocene | NANNO MARL | Dominat lithology; relative abundance | 23 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
699.75 | 12-119-40-1,75 | 0 | 85 | 35 | Upper paleocene | RECRYSTALLIZED NANNO MARL | Dominat lithology; numerical abundance | 53 | 0 | 39 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 |
699.75 | 12-119-40-1,75 | 0 | 85 | 35 | Upper paleocene | RECRYSTALLIZED NANNO MARL | Dominat lithology; relative abundance | 75 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 |
702.75 | 12-119-40-3,75 | 0 | 85 | 35 | Upper paleocene | RECRYSTALLIZED NANNO MARL | Dominat lithology; relative abundance | 75 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
706.60 | 12-119-40-CC,0 | 0 | 85 | 60 | Upper paleocene | RECRYSTALLIZED NANNO MARL | Dominat lithology; relative abundance | 75 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |