Thiede, Jörn; Vallier, Tracy L (2005): Smear slide analysis of Hole 62-465A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230898
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
Vincent, Edith; Windom, Kenneth E; Schmidt, Ronald R; Schaaf, André; Seifert, Karl E; Sayre, W O; Sancetta, Constance A; Rea, David K; Koporulin, V I; Fujii, Naoyuki; Dean, Walter E; Cepek, Pavel; Boersma, Anne; Adelseck, C; Thiede, Jörn; Vallier, Tracy L (1981): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, LXII, 1120 pp, https://doi.org/10.2973/dsdp.proc.62.1981
Further details:
Processed smear slide data base - background and methods. hdl:10013/epic.32353.d001
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 33.820500 * Longitude: 178.919000
Date/Time Start: 1978-08-23T00:00:00 * Date/Time End: 1978-08-23T00:00:00
Minimum DEPTH, sediment/rock: 40.00 m * Maximum DEPTH, sediment/rock: 412.05 m
Event(s):
62-465A * Latitude: 33.820500 * Longitude: 178.919000 * Date/Time: 1978-08-23T00:00:00 * Elevation: -2161.0 m * Penetration: 476 m * Recovery: 98.9 m * Location: North Pacific/CONT RISE * Campaign: Leg62 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 43 cores; 408.5 m cored; 9.5 m drilled; 24.2 % 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 | Siliceous microfossils | Silic foss | % | Smear slide analysis | other siliceous material | |
14 | Chalcedony | Chalcedony | % | Smear slide analysis | ||
15 | Chert | Chert | % | Smear slide analysis | fragments | |
16 | Radiolarians | Rad | % | Smear slide analysis | ||
17 | Barite | Brt | % | Smear slide analysis | ||
18 | Quartz | Qz | % | Smear slide analysis | ||
19 | Feldspar | Fsp | % | Smear slide analysis | ||
20 | Zeolite | Zeo | % | Smear slide analysis | ||
21 | Clay minerals | Clay min | % | Smear slide analysis | ||
22 | Opaque minerals | Opaque | % | Smear slide analysis | ||
23 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
24 | Iron | Fe | % | Smear slide analysis | ||
25 | Heavy minerals | HM | % | Smear slide analysis | ||
26 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
27 | Organic matter | OM | % | Smear slide analysis | organic debris | |
28 | Minerals | Minerals | % | Smear slide analysis | isotropic minerals | |
29 | Micronodules | Micronod | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
2100 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 Silic foss [%] | 14 Chalcedony [%] | 15 Chert [%] | 16 Rad [%] | 17 Brt [%] | 18 Qz [%] | 19 Fsp [%] | 20 Zeo [%] | 21 Clay min [%] | 22 Opaque [%] | 23 Py [%] | 24 Fe [%] | 25 HM [%] | 26 Volc glass [%] | 27 OM [%] | 28 Minerals [%] | 29 Micronod [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
40.00 | 62-465A-1-11,100 | 0 | 0 | 0 | Upper paleocene | NANNO OOZE | Dominat lithology; numerical abundance | 2 | 0 | 95 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
59.00 | 62-465A-3-11,100 | 0 | 0 | 0 | Lower paleocene | NANNO FORAM OOZE | Dominat lithology; relative abundance | 30 | 0 | 10 | 40 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 |
61.15 | 62-465A-3-3,15 | 0 | 0 | 0 | Lower paleocene | NANNO FORAM OOZE | Dominat lithology; relative abundance | 40 | 0 | 10 | 30 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 |
62.43 | 62-465A-3-31,143 | 55 | 20 | 25 | Lower paleocene | PYRITE (COARSE, BLACK MOTTLES) | Minor lithology; relative abundance | 20 | 0 | 5 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 20 | 55 | 0 | 0 | 2 | 0 | 0 | 0 |
62.75 | 62-465A-3-4,25 | 0 | 0 | 0 | Upper maestrichtian | NANNO FORAM OOZE | Minor lithology; relative abundance | 61 | 0 | 10 | 30 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
66.21 | 62-465A-3-CC,5 | 0 | 0 | 0 | Upper maestrichtian | CALCAREOUS OOZE | Dominat lithology; numerical abundance | 75 | 0 | 5 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 |
96.05 | 62-465A-7-1,5 | 0 | 0 | 0 | Upper maestrichtian | NANNO OOZE | Dominat lithology; relative abundance | 5 | 0 | 90 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
105.72 | 62-465A-8-1,22 | 0 | 0 | 0 | Upper maestrichtian | FORAM NANNO OOZE | Dominat lithology; relative abundance | 20 | 0 | 60 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
105.96 | 62-465A-8-CC,8 | 0 | 0 | 0 | Upper maestrichtian | FORAM NANNO OOZE | Minor lithology; numerical abundance | 10 | 0 | 71 | 15 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
115.75 | 62-465A-9-1,75 | 0 | 0 | 0 | Lower maestrichtian | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 10 | 0 | 70 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
123.25 | 62-465A-9-6,75 | 0 | 0 | 0 | Lower maestrichtian | FORAM NANNO OOZE | Dominat lithology; relative abundance | 15 | 0 | 69 | 15 | 0 | 0 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
125.10 | 62-465A-10-1,60 | 0 | 0 | 0 | Lower maestrichtian | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 75 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
128.32 | 62-465A-10-CC,5 | 0 | 0 | 0 | Lower maestrichtian | FORAM NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 85 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
134.60 | 62-465A-11-1,60 | 0 | 0 | 0 | Lower maestrichtian | NANNO OOZE | Dominat lithology; numerical abundance | 15 | 0 | 85 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
137.60 | 62-465A-11-3,60 | 0 | 0 | 0 | Lower maestrichtian | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 91 | 9 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
140.25 | 62-465A-11-CC,5 | 0 | 0 | 0 | Lower maestrichtian | FORAM NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 65 | 25 | 5 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 |
144.30 | 62-465A-12-1,80 | 0 | 0 | 0 | Upper senonian | FORAM NANNO OOZE | Dominat lithology; relative abundance | 40 | 0 | 50 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
146.10 | 62-465A-12-CC,30 | 0 | 0 | 0 | Upper senonian | NANNO OOZE | Dominat lithology; numerical abundance | 50 | 0 | 49 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
173.00 | 62-465A-15-11,100 | 0 | 0 | 0 | Upper campanian | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 85 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
174.35 | 62-465A-15-2,85 | 0 | 0 | 0 | Upper campanian | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 90 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
175.50 | 62-465A-15-3,50 | 0 | 0 | 0 | Upper campanian | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 10 | 0 | 80 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
176.85 | 62-465A-15-4,35 | 0 | 0 | 0 | Upper campanian | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 5 | 0 | 85 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
182.25 | 62-465A-16-1,75 | 0 | 0 | 0 | Upper campanian | NANNO OOZE | Dominat lithology; numerical abundance | 15 | 0 | 80 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
183.75 | 62-465A-16-2,75 | 0 | 0 | 0 | Upper campanian | NANNO OOZE | Dominat lithology; relative abundance | 10 | 0 | 90 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
185.25 | 62-465A-16-3,75 | 0 | 0 | 0 | Upper campanian | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 10 | 0 | 80 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
186.75 | 62-465A-16-4,75 | 0 | 0 | 0 | Upper campanian | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 5 | 0 | 83 | 12 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
191.60 | 62-465A-17-1,60 | 0 | 0 | 0 | Upper campanian | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 8 | 0 | 72 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
192.75 | 62-465A-17-2,25 | 0 | 0 | 0 | Upper campanian | NANNO OOZE | Minor lithology; relative abundance | 5 | 0 | 90 | 5 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
201.25 | 62-465A-18-1,75 | 0 | 0 | 0 | Upper campanian | NANNO OOZE | Dominat lithology; numerical abundance | 15 | 0 | 77 | 8 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
202.20 | 62-465A-18-2,20 | 0 | 0 | 0 | Upper campanian | NANNO FORAM CHALK | Dominat lithology; numerical abundance | 8 | 0 | 57 | 35 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
210.24 | 62-465A-19-1,24 | 0 | 0 | 0 | Upper campanian | NANNO OOZE | Dominat lithology; numerical abundance | 15 | 0 | 76 | 9 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
213.20 | 62-465A-19-3,20 | 0 | 0 | 0 | Upper campanian | NANNO OOZE | Dominat lithology; numerical abundance | 5 | 0 | 87 | 8 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
220.45 | 62-465A-20-1,95 | 0 | 0 | 0 | Upper campanian | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 10 | 0 | 65 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
223.87 | 62-465A-20-31,137 | 0 | 0 | 0 | Santonian | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 15 | 0 | 55 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
229.45 | 62-465A-21-1,45 | 0 | 0 | 0 | Santonian | NANNO OOZE | Dominat lithology; numerical abundance | 5 | 0 | 85 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
233.75 | 62-465A-21-4,25 | 0 | 0 | 0 | Santonian | FORAM NANNO OOZE (GREENISH GRAY) | Minor lithology; numerical abundance | 0 | 0 | 85 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
234.45 | 62-465A-21-4,95 | 0 | 0 | 0 | Santonian | FORAM NANNO OOZE | Dominat lithology; relative abundance | 40 | 0 | 50 | 10 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
234.77 | 62-465A-21-CC,0 | 0 | 0 | 0 | Santonian | FORAM NANNO OOZE | Dominat lithology; relative abundance | 20 | 0 | 42 | 23 | 0 | 0 | 0 | 10 | 0 | 5 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
248.09 | 62-465A-23-CC,9 | 0 | 0 | 0 | Santonian | NANNO OOZE | Dominat lithology; relative abundance | 20 | 0 | 61 | 9 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
276.65 | 62-465A-26-1,15 | 0 | 0 | 0 | Lower cenomanian | NANNO OOZE | Dominat lithology; numerical abundance | 51 | 0 | 40 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 3 |
277.30 | 62-465A-26-1,80 | 0 | 0 | 0 | Lower cenomanian | LIMESTONE | Dominat lithology; relative abundance | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
277.45 | 62-465A-26-1,95 | 0 | 0 | 0 | Lower cenomanian | CLAYEY CHERT (DARK GRAY) | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
277.85 | 62-465A-26-CC,0 | 0 | 0 | 0 | Lower cenomanian | CLAY INSOLUBLE FRACT. | Dominat lithology; numerical abundance | 5 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 80 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 |
286.80 | 62-465A-27-1,80 | 0 | 0 | 0 | Lower cenomanian | LIMESTONE (RECRYSTALLIZED) | Dominat lithology; numerical abundance | 97 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 |
288.15 | 62-465A-27-2,65 | 0 | 0 | 0 | Lower cenomanian | CALCITE VEIN | Minor lithology; numerical abundance | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
288.83 | 62-465A-27-21,133 | 0 | 0 | 0 | Lower cenomanian | NANNO OOZE | Dominat lithology; relative abundance | 36 | 0 | 30 | 8 | 0 | 0 | 0 | 0 | 0 | 10 | 1 | 5 | 5 | 2 | 0 | 2 | 0 | 3 | 0 | 0 | 0 |
295.70 | 62-465A-28-1,20 | 0 | 0 | 0 | Upper albian | LIMESTONE RECRYSTALLIZED (GREEN) | Dominat lithology; numerical abundance | 90 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
296.10 | 62-465A-28-1,60 | 0 | 0 | 0 | Upper albian | NANNO OOZE (DARK GREEN) | Minor lithology; relative abundance | 0 | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
297.20 | 62-465A-28-2,20 | 0 | 0 | 0 | Upper albian | RECRYSTALLIZED LIMESTONE (DARK) | Minor lithology; numerical abundance | 93 | 0 | 0 | 7 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
305.45 | 62-465A-29-1,45 | 0 | 0 | 0 | Upper albian | NANNO CHALK | Dominat lithology; relative abundance | 60 | 0 | 35 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 0 |
306.38 | 62-465A-29-11,138 | 0 | 0 | 0 | Upper albian | NANNO LIMESTONE | Dominat lithology; relative abundance | 85 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
306.51 | 62-465A-29-2,1 | 0 | 0 | 0 | Upper albian | FORAM NANNO OOZE (COARSE) | Dominat lithology; relative abundance | 25 | 0 | 53 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
314.70 | 62-465A-30-1,20 | 0 | 0 | 0 | Upper albian | NANNO OOZE (SOFT) | Minor lithology; numerical abundance | 2 | 0 | 78 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
315.15 | 62-465A-30-1,65 | 0 | 0 | 0 | Upper albian | RECRYSTALLIZED LIMESTONE (GREENISH) | Dominat lithology; numerical abundance | 90 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
324.22 | 62-465A-31-1,22 | 0 | 0 | 0 | Upper albian | NANNO OOZE (PARTLY RECRYSTALLIZED) | Minor lithology; numerical abundance | 25 | 0 | 65 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 |
333.65 | 62-465A-32-1,15 | 0 | 0 | 0 | Upper albian | RECRYSTALLIZED FORAM LIMESTONE | Dominat lithology; numerical abundance | 70 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
333.85 | 62-465A-32-1,35 | 0 | 0 | 0 | Upper albian | CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 85 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 |
334.29 | 62-465A-32-1,79 | 0 | 0 | 0 | Upper albian | LIMESTONE (COARSELY REXTALLIZED) GRAY | Dominat lithology; numerical abundance | 92 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 0 | 0 | 0 | 0 | 0 |
343.30 | 62-465A-33-1,30 | 0 | 0 | 0 | Upper albian | RECRYSTALLIZED LIMESTONE (VERY DARK) | Minor lithology; numerical abundance | 92 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 |
343.55 | 62-465A-33-1,55 | 0 | 0 | 0 | Upper albian | RECRYSTALLIZED FORAM LIMESTONE (GREEN.)M CARB 75 | Dominat lithology; numerical abundance | 0 | 0 | 0 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
381.70 | 62-465A-37-1,70 | 0 | 0 | 0 | Upper albian | RECRYSTALLIZED CARBONATE | Dominat lithology; numerical abundance | 95 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
382.25 | 62-465A-37-11,125 | 0 | 0 | 0 | Upper albian | RECRYSTALLIZED CARBONATE (DARK GRAY) | Minor lithology; numerical abundance | 85 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 8 | 0 | 0 | 0 | 0 | 0 | 0 |
383.32 | 62-465A-37-2,82 | 0 | 0 | 0 | Upper albian | FORAM LIMESTONE | Minor lithology; relative abundance | 60 | 0 | 10 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
392.89 | 62-465A-38-2,89 | 0 | 0 | 0 | Upper albian | RECRYSTALLIZED LIMESTONE | Dominat lithology; numerical abundance | 80 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
400.83 | 62-465A-39-1,83 | 0 | 0 | 0 | Upper albian | RECRYSTALLIZED LIMESTONE (GREEN) | Dominat lithology; numerical abundance | 97 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
410.61 | 62-465A-40-11,111 | 0 | 0 | 0 | Upper albian | BLACK COATING OF GRAINS | Minor lithology; numerical abundance | 68 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 10 | 0 | 5 | 0 | 0 | 15 | 0 | 0 | 0 |
410.69 | 62-465A-40-11,119 | 0 | 0 | 0 | Upper albian | COAL OR BLACK SHALE | Minor lithology; relative abundance | 25 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 10 | 0 | 5 | 0 | 0 | 5 | 45 | 0 | 0 |
410.79 | 62-465A-40-11,129 | 0 | 0 | 0 | Upper albian | CALCAREOUS CLAY | Minor lithology; relative abundance | 15 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 1 | 64 | 0 | 1 | 0 | 2 | 10 | 0 | 0 | 0 |
410.88 | 62-465A-40-11,138 | 0 | 0 | 0 | Upper albian | MARLY LIMESTONE | Dominat lithology; numerical abundance | 15 | 0 | 2 | 5 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 25 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
410.88 | 62-465A-40-11,138 | 0 | 0 | 0 | Upper albian | RECRYSTALLIZED LIMESTONE (GRN. GRAY) | Dominat lithology; relative abundance | 93 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 |
411.50 | 62-465A-40-2,50 | 0 | 0 | 0 | Upper albian | ASHY CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 75 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 |
411.60 | 62-465A-40-2,60 | 0 | 0 | 0 | Upper albian | CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 75 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 |
411.64 | 62-465A-40-2,64 | 0 | 0 | 0 | Upper albian | TUFF | Dominat lithology; numerical abundance | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 74 | 0 | 3 | 0 | 0 | 2 | 0 | 0 | 0 |
411.89 | 62-465A-40-2,89 | 0 | 0 | 0 | Upper albian | BARITE (PINK) | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 90 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
412.05 | 62-465A-40-21,105 | 0 | 0 | 0 | Upper albian | TUFF | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 87 | 0 | 2 | 0 | 0 | 8 | 0 | 0 | 0 |