Thiede, Jörn; Vallier, Tracy L (2005): Smear slide analysis of Hole 62-464 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230896
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: 39.860700 * Longitude: 173.888800
Date/Time Start: 1978-08-17T00:00:00 * Date/Time End: 1978-08-17T00:00:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 288.77 m
Event(s):
62-464 * Latitude: 39.860700 * Longitude: 173.888800 * Date/Time: 1978-08-17T00:00:00 * Elevation: -4637.0 m * Penetration: 308.5 m * Recovery: 77.6 m * Location: North Pacific/CONT RISE * Campaign: Leg62 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 34 cores; 308.5 m cored; 0 m drilled; 25.2 % 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 | Nannofossils | Nannos | % | Smear slide analysis | ||
11 | Siliceous microfossils | Silic foss | % | Smear slide analysis | other siliceous material | |
12 | Radiolarians | Rad | % | Smear slide analysis | ||
13 | Diatoms | Diatoms | % | Smear slide analysis | ||
14 | Silicoflagellates | Silicoflag | % | Smear slide analysis | ||
15 | Spiculae | Spiculae | % | Smear slide analysis | ||
16 | Quartz | Qz | % | Smear slide analysis | ||
17 | Feldspar | Fsp | % | Smear slide analysis | ||
18 | Zeolite | Zeo | % | Smear slide analysis | ||
19 | Mica | Mica | % | Smear slide analysis | ||
20 | Clay minerals | Clay min | % | Smear slide analysis | ||
21 | Glauconite | Glt | % | 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 | Terrigenous | Terr | % | Smear slide analysis | terrigeneous detritus | |
28 | Micronodules | Micronod | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1742 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 Nannos [%] | 11 Silic foss [%] | 12 Rad [%] | 13 Diatoms [%] | 14 Silicoflag [%] | 15 Spiculae [%] | 16 Qz [%] | 17 Fsp [%] | 18 Zeo [%] | 19 Mica [%] | 20 Clay min [%] | 21 Glt [%] | 22 Opaque [%] | 23 Py [%] | 24 Fe [%] | 25 HM [%] | 26 Volc glass [%] | 27 Terr [%] | 28 Micronod [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.01 | 62-464-1-1,1 | 0 | 0 | 0 | Lower pleistocene | ASH | Minor lithology; relative abundance | 0 | 2 | 0 | 5 | 5 | 0 | 2 | 0 | 21 | 0 | 0 | 45 | 0 | 2 | 0 | 0 | 0 | 20 | 0 | 0 |
4.45 | 62-464-2-1,95 | 0 | 0 | 0 | Upper pliocene | CLAYEY SILICEOUS OOZE (CLAY BALL) | Minor lithology; relative abundance | 15 | 20 | 0 | 15 | 7 | 2 | 2 | 1 | 0 | 0 | 0 | 40 | 0 | 0 | 0 | 4 | 0 | 0 | 1 | 0 |
5.63 | 62-464-2-2,63 | 0 | 0 | 0 | Upper pliocene | CLAYEY RADS OOZE | Dominat lithology; relative abundance | 5 | 5 | 0 | 20 | 15 | 2 | 5 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
6.10 | 62-464-2-21,110 | 0 | 0 | 0 | Upper pliocene | CLAYEY RAD OOZE | Dominat lithology; relative abundance | 1 | 5 | 0 | 26 | 12 | 2 | 3 | 0 | 0 | 0 | 0 | 50 | 2 | 2 | 0 | 2 | 0 | 2 | 0 | 1 |
6.30 | 62-464-2-21,130 | 0 | 0 | 0 | Upper pliocene | DIATOM RAD OOZE | Dominat lithology; relative abundance | 2 | 2 | 0 | 40 | 22 | 1 | 2 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 1 |
6.52 | 62-464-2-3,2 | 0 | 0 | 0 | Upper pliocene | RAD CLAY | Dominat lithology; numerical abundance | 2 | 2 | 0 | 10 | 5 | 1 | 1 | 1 | 1 | 0 | 1 | 75 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
6.70 | 62-464-2-3,20 | 0 | 0 | 0 | Upper pliocene | CLAYEY RADS OOZE GREEN PATCH | Minor lithology; numerical abundance | 10 | 5 | 0 | 25 | 7 | 0 | 3 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
10.92 | 62-464-2-51,142 | 0 | 0 | 0 | Upper pliocene | CLAYEY RAD OOZE | Dominat lithology; numerical abundance | 2 | 2 | 0 | 30 | 15 | 1 | 5 | 1 | 0 | 0 | 0 | 40 | 1 | 0 | 0 | 0 | 0 | 2 | 1 | 0 |
11.15 | 62-464-2-6,15 | 0 | 0 | 0 | Lower pliocene | SILICEOUS CLAY | Dominat lithology; numerical abundance | 0 | 6 | 0 | 10 | 10 | 2 | 0 | 0 | 0 | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
12.95 | 62-464-2-7,45 | 0 | 0 | 0 | Lower pliocene | CLAYEY RADS OOZE BROWN | Dominat lithology; relative abundance | 2 | 0 | 0 | 25 | 10 | 0 | 5 | 5 | 5 | 0 | 2 | 55 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
13.07 | 62-464-2-CC,0 | 0 | 0 | 0 | Lower pliocene | DIATOM RADS OOZE | Dominat lithology; relative abundance | 1 | 10 | 0 | 45 | 24 | 2 | 3 | 5 | 0 | 0 | 0 | 15 | 2 | 2 | 0 | 4 | 0 | 2 | 0 | 0 |
13.23 | 62-464-3-1,23 | 0 | 0 | 0 | Lower pliocene | CLAYEY RADS OOZE BROWN | Minor lithology; relative abundance | 5 | 0 | 0 | 25 | 10 | 0 | 10 | 5 | 5 | 0 | 0 | 45 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
14.45 | 62-464-3-11,145 | 0 | 0 | 0 | Lower pliocene | CLAYEY SILICEOUS OOZE | Dominat lithology; numerical abundance | 2 | 5 | 0 | 20 | 16 | 1 | 5 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
16.70 | 62-464-3-3,70 | 0 | 0 | 0 | Lower pliocene | CLAYEY RADS OOZE GREEN | Dominat lithology; numerical abundance | 10 | 0 | 0 | 20 | 10 | 0 | 10 | 5 | 5 | 0 | 0 | 45 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
21.20 | 62-464-3-6,70 | 0 | 0 | 0 | Lower pliocene | SILICEOUS CLAY | Dominat lithology; relative abundance | 2 | 0 | 0 | 12 | 12 | 2 | 1 | 0 | 1 | 0 | 0 | 74 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 |
23.00 | 62-464-4-1,50 | 0 | 0 | 0 | Lower pliocene | SILICEOUS CLAY (GREEN) | Dominat lithology; relative abundance | 0 | 0 | 0 | 15 | 9 | 0 | 5 | 0 | 0 | 0 | 0 | 71 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
23.12 | 62-464-4-1,62 | 0 | 0 | 0 | Lower pliocene | SILICEOUS CLAY (INTERVAL PART OF MN) | Minor lithology; numerical abundance | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
23.52 | 62-464-4-11,102 | 0 | 0 | 0 | Lower pliocene | NANNO DIATOM OOZE | Minor lithology; numerical abundance | 0 | 20 | 0 | 15 | 25 | 1 | 1 | 2 | 2 | 0 | 0 | 35 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 |
23.52 | 62-464-4-11,102 | 0 | 0 | 0 | Lower pliocene | NANNO DIATOM OOZE (WHITE MOTTLE) | Minor lithology; relative abundance | 0 | 25 | 0 | 5 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 2 |
24.30 | 62-464-4-2,30 | 0 | 0 | 0 | Lower pliocene | SILICEOS CLAY | Dominat lithology; relative abundance | 2 | 0 | 0 | 18 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 72 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
25.00 | 62-464-4-21,100 | 0 | 0 | 0 | Lower pliocene | SILICEOUS CLAY (LIGHT BROWNISH YELLOW) | Dominat lithology; relative abundance | 0 | 0 | 0 | 15 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 75 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
28.90 | 62-464-4-5,40 | 0 | 0 | 0 | Lower pliocene | SILICEOUS CLAY (GREEN) | Dominat lithology; relative abundance | 0 | 2 | 0 | 15 | 10 | 0 | 0 | 2 | 2 | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
32.50 | 62-464-5-1,50 | 0 | 0 | 0 | Neogene | SILICEOUS CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 15 | 10 | 2 | 0 | 2 | 2 | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
37.00 | 62-464-5-4,50 | 0 | 0 | 0 | Neogene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 0 | 90 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 5 |
39.24 | 62-464-5-CC,0 | 0 | 0 | 0 | Neogene | PELAGIC CLAY (BROWN) | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 3 | 10 | 0 | 67 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 15 |
42.30 | 62-464-6-1,80 | 1 | 5 | 95 | Tertiary | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 1 | 0 | 92 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 5 |
48.30 | 62-464-6-5,80 | 1 | 3 | 97 | Lower eocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 2 | 0 | 95 | 0 | 1 | 0 | 2 | 0 | 2 | 0 | 2 |
49.90 | 62-464-6-6,90 | 0 | 0 | 0 | Lower eocene | CLAYSTONE (CLAYSTONE FRAG IN CLAY) | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 98 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 |
51.80 | 62-464-7-1,80 | 0 | 0 | 0 | Paleocene | CLAY (PELAGIC) REDDISH BROWN | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 88 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 10 |
54.80 | 62-464-7-3,80 | 0 | 0 | 0 | Paleocene | BRICKSTONE CONCRETION | Minor lithology; relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 97 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 |
58.35 | 62-464-7-51,135 | 0 | 0 | 0 | Paleocene | CARBONATE CRYSTALS (LARGE XTALS) | Minor lithology; numerical abundance | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 28 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
59.70 | 62-464-7-61,120 | 0 | 0 | 0 | Paleocene | CLAY (PELAGIC) (W/GREENISH GRAY TINT) | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 95 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 5 |
60.99 | 62-464-8-1,49 | 0 | 0 | 0 | Paleocene | CLAY (PELAGIC) | Dominat lithology; relative abundance | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 85 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 5 |
70.75 | 62-464-9-1,75 | 0 | 0 | 0 | Upper cretaceous | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 97 | 0 | 2 |
81.80 | 62-464-10-2,80 | 0 | 0 | 0 | Upper cretaceous | ZEOLITIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 20 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 |
82.84 | 62-464-10-3,34 | 0 | 0 | 0 | Upper cretaceous | PHILLIPSITE NODULE | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 95 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
89.18 | 62-464-11-1,18 | 0 | 0 | 0 | Cenomanian | PORCELLANITE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 20 | 0 | 25 | 0 | 0 | 0 | 0 | 0 | 0 |
89.75 | 62-464-11-1,75 | 0 | 0 | 0 | Cenomanian | SILICIFIED LIMESTONE | Dominat lithology; numerical abundance | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
98.70 | 62-464-12-1,20 | 0 | 0 | 0 | Cenomanian | LIMESTONE (GREENISH GREY) | Dominat lithology; relative abundance | 85 | 10 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
99.00 | 62-464-12-1,50 | 0 | 0 | 0 | Cenomanian | NANNO LIMESTONE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
99.00 | 62-464-12-1,50 | 10 | 10 | 80 | Cenomanian | RECRYSTALLIZED SIO2 | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
100.00 | 62-464-12-1,50 | 70 | 20 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | ||||||
100.00 | 62-464-12-1,50 | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | ||||||
108.10 | 62-464-13-CC,0 | 0 | 0 | 0 | Cenomanian | LIMESTONE | Dominat lithology; numerical abundance | 65 | 5 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
117.57 | 62-464-14-1,7 | 0 | 0 | 0 | Cenomanian | LIMESTONE | Dominat lithology; numerical abundance | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 35 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 |
127.10 | 62-464-15-CC,0 | 0 | 0 | 0 | Cenomanian | NANNO LIMESTONE | Dominat lithology; numerical abundance | 55 | 40 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
136.60 | 62-464-16-CC,0 | 0 | 0 | 0 | Cenomanian | LIMESTONE | Dominat lithology; numerical abundance | 45 | 20 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
146.30 | 62-464-17-CC,30 | 0 | 0 | 0 | Cretaceous | LIMESTONE (WHITE COATING OF CHERT) | Minor lithology; numerical abundance | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
155.63 | 62-464-18-CC,13 | 0 | 0 | 0 | Cretaceous | LIMESTONE (WHITE COATING OF CHERT) | Minor lithology; numerical abundance | 75 | 5 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 |
174.94 | 62-464-20-1,44 | 0 | 0 | 0 | Upper albian | LIMESTONE | Minor lithology; numerical abundance | 80 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
184.10 | 62-464-21-1,10 | 0 | 0 | 0 | Upper albian | SILICEOUS MARLSTONE | Dominat lithology; numerical abundance | 58 | 2 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 |
184.10 | 62-464-21-1,10 | 0 | 0 | 0 | Upper albian | SILICEOUS MARLSTONE | Dominat lithology; numerical abundance | 75 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
203.27 | 62-464-23-1,27 | 0 | 0 | 0 | Upper albian | CHALK | Minor lithology; numerical abundance | 65 | 20 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
212.76 | 62-464-24-CC,26 | 0 | 0 | 0 | Albian | CHALK (PINKISH COATING OF CHERT FRAG) | Minor lithology; numerical abundance | 70 | 20 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
222.57 | 62-464-25-1,57 | 0 | 0 | 0 | Albian | CHALK (COATING OF CHERT FRAG) | Minor lithology; relative abundance | 96 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
232.13 | 62-464-26-1,63 | 0 | 0 | 0 | Lower albian | CHALK (CAVITY OF CHERT FRAG) | Minor lithology; numerical abundance | 60 | 40 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
241.43 | 62-464-27-1,43 | 0 | 0 | 0 | Lower cretaceous | RAD NANNOFOSSIL CHALK | Dominat lithology; numerical abundance | 25 | 60 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
260.26 | 62-464-29-1,26 | 0 | 0 | 0 | Lower cretaceous | CLAY (RED SEDIMENT ON CHERT) | Minor lithology; relative abundance | 5 | 2 | 15 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 78 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 |
260.42 | 62-464-29-1,42 | 0 | 0 | 0 | Lower cretaceous | Minor lithology; numerical abundance | 10 | 5 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | |
260.66 | 62-464-29-1,66 | 0 | 0 | 0 | Lower cretaceous | NANNO MARLSTONE | Dominat lithology; numerical abundance | 20 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 53 | 0 | 4 | 0 | 0 | 0 | 3 | 0 | 0 |
260.96 | 62-464-29-1,96 | 0 | 0 | 0 | Lower cretaceous | RED SEIDMENT ON CHERT | Minor lithology; relative abundance | 5 | 0 | 20 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 72 | 0 | 1 | 0 | 1 | 0 | 2 | 0 | 1 |
269.73 | 62-464-30-1,23 | 0 | 0 | 0 | Lower cretaceous | CLAY (YELLOW SEDIMENT ON CHERT) | Minor lithology; relative abundance | 0 | 1 | 8 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 89 | 0 | 1 | 0 | 1 | 0 | 2 | 0 | 2 |
269.83 | 62-464-30-1,33 | 0 | 0 | 0 | Lower cretaceous | CLAY (YELLOW SEDIMENT ON CHERT) | Minor lithology; relative abundance | 10 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 85 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 |
288.75 | 62-464-32-1,25 | 0 | 0 | 0 | Lower cretaceous | RED | Dominat lithology; numerical abundance | 5 | 30 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 |
288.77 | 62-464-32-1,27 | 0 | 0 | 0 | Lower cretaceous | CLAY INSOLUBLE IN HCL FRACTION | Dominat lithology; relative abundance | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 80 | 0 | 0 | 0 | 10 | 0 | 5 | 0 | 0 |