Larson, Roger L; Schlanger, Seymour O (2005): Smear slide analysis of Hole 61-462A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230894
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
Windom, Ken; Vallier, Tracy L; Tokuyama, Hidekazu; Thierstein, Hans R; Thiede, Jörn; Steiner, Maureen B; Sliter, William V; Shcheka, S A; Seifert, Karl E; Sayer, William O; Riech, Volkher; Rea, David K; Premoli Silva, Isabella; Moberly, Ralph; Koporulin, V I; Jenkyns, Hugh C; Fujii, Naoyuki; de Wever, Patrick; Cepek, Pavel; Boyce, Robert E; Batiza, Rodey; Larson, Roger L; Schlanger, Seymour O (1981): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, LXI, 885 pp, https://doi.org/10.2973/dsdp.proc.61.1981
Further details:
Processed smear slide data base - background and methods. hdl:10013/epic.32353.d001
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 7.241700 * Longitude: 165.031700
Date/Time Start: 1978-06-09T00:00:00 * Date/Time End: 1978-06-09T00:00:00
Minimum DEPTH, sediment/rock: 84.00 m * Maximum DEPTH, sediment/rock: 992.62 m
Event(s):
61-462A * Latitude: 7.241700 * Longitude: 165.031700 * Date/Time: 1978-06-09T00:00:00 * Elevation: -5177.0 m * Penetration: 1068.5 m * Recovery: 344 m * Campaign: Leg61 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 90 cores; 619.5 m cored; 14.5 m drilled; 55.5 % 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 | Foraminifera | Foram | % | Smear slide analysis | ||
12 | Opal, biogenic silica | bSiO2 | % | Smear slide analysis | ||
13 | Radiolarians | Rad | % | Smear slide analysis | ||
14 | Diatoms | Diatoms | % | Smear slide analysis | ||
15 | Silicoflagellates | Silicoflag | % | Smear slide analysis | ||
16 | Spiculae | Spiculae | % | Smear slide analysis | ||
17 | Quartz | Qz | % | Smear slide analysis | ||
18 | Feldspar | Fsp | % | Smear slide analysis | ||
19 | Zeolite | Zeo | % | Smear slide analysis | ||
20 | Clay minerals | Clay min | % | Smear slide analysis | ||
21 | Opaque minerals | Opaque | % | Smear slide analysis | ||
22 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
23 | Iron | Fe | % | Smear slide analysis | ||
24 | Magnetite | Fe3O4 | % | Smear slide analysis | ||
25 | Heavy minerals | HM | % | Smear slide analysis | ||
26 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
27 | Palagonite | Palagonite | % | Smear slide analysis | ||
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:
2155 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 Foram [%] | 12 bSiO2 [%] | 13 Rad [%] | 14 Diatoms [%] | 15 Silicoflag [%] | 16 Spiculae [%] | 17 Qz [%] | 18 Fsp [%] | 19 Zeo [%] | 20 Clay min [%] | 21 Opaque [%] | 22 Py [%] | 23 Fe [%] | 24 Fe3O4 [%] | 25 HM [%] | 26 Volc glass [%] | 27 Palagonite [%] | 28 Minerals [%] | 29 Micronod [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
84.00 | 61-462A-1-41,100 | 49 | 26 | 25 | Miocene | NANNOFOSSIL FORAMINIFERAL OOZE | Dominat lithology; relative abundance | 0 | 50 | 49 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
84.20 | 61-462A-1-41,120 | 2 | 93 | 5 | Miocene | RADIOLARIAN OOZE | Dominat lithology; numerical abundance | 0 | 1 | 0 | 0 | 86 | 3 | 0 | 5 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
86.49 | 61-462A-1-6,49 | 8 | 12 | 80 | Miocene | NANNOFOSSIL OOZE | Dominat lithology; numerical abundance | 0 | 87 | 3 | 0 | 3 | 2 | 1 | 1 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
88.08 | 61-462A-1-CC,0 | 15 | 45 | 15 | NANNOFOSSIL FORAMINIFERAL OOZE | Dominat lithology; relative abundance | 0 | 1 | 45 | 0 | 2 | 4 | 2 | 2 | 0 | 2 | 0 | 10 | 0 | 0 | 1 | 0 | 0 | 2 | 2 | 0 | 0 | |
88.08 | 61-462A-1-CC,0 | 30 | 55 | 40 | RADIOLARIAN OOZE | Dominat lithology; relative abundance | 0 | 52 | 0 | 0 | 78 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
250.39 | 61-462A-2-1,89 | 15 | 55 | 30 | Lower tertiary | NANNOFOSSIL RADIOLARIAN OOZE | Dominat lithology; relative abundance | 0 | 45 | 0 | 0 | 49 | 0 | 0 | 2 | 0 | 0 | 0 | 5 | 0 | 0 | 1 | 0 | 0 | 2 | 1 | 0 | 0 |
250.75 | 61-462A-2-11,125 | 2 | 65 | 33 | Lower tertiary | NANNOFOSSIL CHALK | Dominat lithology; relative abundance | 0 | 80 | 0 | 0 | 19 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 |
251.30 | 61-462A-2-2,30 | 5 | 70 | 25 | Lower tertiary | NANNO-BEARING RADIOLARIAN OOZE | Minor lithology; relative abundance | 0 | 15 | 3 | 0 | 60 | 0 | 0 | 8 | 0 | 0 | 0 | 10 | 0 | 0 | 2 | 0 | 0 | 0 | 4 | 0 | 0 |
257.83 | 61-462A-2-CC,0 | 2 | 75 | 23 | Lower tertiary | NANNOFOSSIL OOZE | Dominat lithology; relative abundance | 0 | 80 | 10 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 |
411.15 | 61-462A-4-1,15 | 0 | 0 | 0 | Lower eocene | LIMESTONE | Dominat lithology; relative abundance | 93 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 5 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
439.53 | 61-462A-7-1,3 | 0 | 0 | 0 | Middle maestrichtian | POCELLANITE W/ QTZ-FILLED MICROFOSSILS | Minor lithology; numerical abundance | 3 | 0 | 0 | 87 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
440.05 | 61-462A-7-1,55 | 0 | 0 | 0 | Middle maestrichtian | ZEOLITIC CALCARENITE | Dominat lithology; relative abundance | 87 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 |
440.50 | 61-462A-7-11,100 | 0 | 0 | 0 | Middle maestrichtian | ZEOLITIC LIMESTONE | Dominat lithology; numerical abundance | 73 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 15 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
440.55 | 61-462A-7-11,105 | 0 | 0 | 0 | Middle maestrichtian | ZEOLITIC CALCARENITE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
440.77 | 61-462A-7-11,127 | 0 | 0 | 0 | Middle maestrichtian | LIMESTONE W. QUARTZOSE CHERT STRINGERS | Minor lithology; numerical abundance | 85 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 10 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
487.80 | 61-462A-8-1,80 | 0 | 25 | 75 | Upper campanian | MARLY NANNOFOSSIL LIMESTONE | Dominat lithology; relative abundance | 50 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 15 | 0 | 0 | 0 | 0 | 4 | 2 | 1 | 0 | 0 |
488.92 | 61-462A-8-2,42 | 70 | 20 | 10 | Upper campanian | VOLCANIC SANDSTONE | Minor lithology; numerical abundance | 4 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 15 | 70 | 0 | 0 | 0 |
490.55 | 61-462A-8-3,55 | 0 | 20 | 80 | Upper campanian | LIMESTONE | Dominat lithology; relative abundance | 85 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 0 |
516.44 | 61-462A-9-1,94 | 3 | 27 | 70 | Lower campanian | ZEOLITIC CLAYSTONE | Dominat lithology; relative abundance | 2 | 2 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 30 | 70 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
516.90 | 61-462A-9-11,140 | 0 | 0 | 0 | Lower campanian | ZEOLITIC LIMESTONE | Dominat lithology; relative abundance | 80 | 2 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 10 | 5 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
517.60 | 61-462A-9-2,60 | 0 | 15 | 85 | Lower campanian | CLAYSTONE | Dominat lithology; relative abundance | 5 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 81 | 0 | 1 | 2 | 0 | 2 | 3 | 0 | 0 | 0 |
522.10 | 61-462A-9-5,60 | 0 | 0 | 0 | Lower campanian | ZEOLITIC CLAYSTONE | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 50 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 |
522.61 | 61-462A-9-51,111 | 0 | 0 | 0 | Lower campanian | ZEOLITIC CLAYSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 20 | 77 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
523.32 | 61-462A-9-6,32 | 0 | 0 | 0 | Lower campanian | ZEOLITIC CLAYSTONE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
527.40 | 61-462A-10-2,90 | 0 | 2 | 98 | CLAYSTONE | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 96 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | |
527.50 | 61-462A-10-21,100 | 0 | 8 | 92 | CLAYSTONE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 2 | 92 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | |
529.19 | 61-462A-10-31,119 | 0 | 90 | 10 | VOLCANICLASTIC SILTSTONE (HYALOCLASTIC)M FEL 3,CLAY 10,VOLC.GLAS 84/N AL | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
529.60 | 61-462A-10-4,10 | 0 | 0 | 0 | ZEOLITIC CLAYSTONE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 37 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | |
529.85 | 61-462A-10-CC,0 | 0 | 90 | 10 | VOLCANICLASTIC SILTSTONE | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 10 | 5 | 0 | 0 | 0 | 0 | 0 | 82 | 0 | 0 | 0 | |
535.45 | 61-462A-11-1,95 | 0 | 100 | 0 | Upper santonian | ZEOLITIC VOLCANOCLASTIC SILTSTONE | Dominat lithology; relative abundance | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 1 | 40 | 0 | 0 | 0 | 2 | 0 | 0 | 39 | 0 | 0 | 0 |
535.92 | 61-462A-11-11,142 | 0 | 100 | 0 | Upper santonian | VOLCANOCLASTIC VITRIC SILTSTONE | Dominat lithology; relative abundance | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 83 | 0 | 0 | 0 |
536.22 | 61-462A-11-2,22 | 0 | 20 | 80 | Upper santonian | CALCAREOUS CLAYSTONE | Dominat lithology; relative abundance | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 3 | 73 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 |
544.30 | 61-462A-12-1,30 | 0 | 0 | 0 | Cretaceous | RADIOLARIAN CLAYSTONE | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 5 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
545.52 | 61-462A-12-2,2 | 5 | 13 | 82 | Cretaceous | RADIOLARIAN CLAYSTONE | Dominat lithology; numerical abundance | 2 | 1 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 3 | 81 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 |
553.10 | 61-462A-13-1,10 | 0 | 0 | 0 | Cretaceous | SLIGHTLY CALCAREOUS CLAYSTONE | Dominat lithology; numerical abundance | 5 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 80 | 0 | 0 | 0 | 0 | 1 | 5 | 0 | 0 | 0 |
554.00 | 61-462A-13-11,100 | 0 | 0 | 0 | Cretaceous | ZEOLITIC CLAYSTONE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 88 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 0 |
554.52 | 61-462A-13-2,2 | 80 | 5 | 15 | Cretaceous | RADIOLARIAN SAND LAYER | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 80 | 0 | 0 | 0 | 0 | 1 | 0 | 14 | 0 | 0 | 2 | 0 | 0 | 5 | 0 | 0 | 0 |
554.60 | 61-462A-13-2,10 | 0 | 10 | 90 | Cretaceous | ZEOLITIC CLAYSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 80 | 0 | 0 | 2 | 0 | 2 | 10 | 0 | 0 | 0 |
555.70 | 61-462A-13-21,120 | 0 | 20 | 80 | Cretaceous | ZEOLITIC CLAYSTONE | Dominat lithology; numerical abundance | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 74 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 |
556.02 | 61-462A-13-3,2 | 0 | 0 | 100 | Cretaceous | CLAYSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
563.70 | 61-462A-14-1,70 | 0 | 0 | 0 | RADIOLARIANS CLAYSTONE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 1 | 5 | 87 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | |
564.01 | 61-462A-14-11,101 | 4 | 1 | 95 | CLAYSTONE | Dominat lithology; relative abundance | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 5 | 92 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | |
566.53 | 61-462A-15-1,3 | 0 | 80 | 20 | VOLCANIC ZEOLITIC MUDSTONE | Minor lithology; numerical abundance | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 85 | 0 | 0 | 0 | |
566.58 | 61-462A-15-1,8 | 15 | 70 | 15 | VOLCANIC ZEOLITIC MUDSTONE | Minor lithology; numerical abundance | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 93 | 0 | 0 | 0 | |
589.90 | 61-462A-22-2,40 | 80 | 10 | 10 | VOLCANOCLASTIC SANDSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 10 | 10 | 0 | 0 | 0 | 0 | 2 | 60 | 0 | 0 | 0 | |
599.27 | 61-462A-23-2,77 | 15 | 85 | 0 | VOLCANOCLASTIC SILTSTONE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 70 | 0 | 0 | 0 | 0 | 0 | 10 | 5 | 0 | 0 | 0 | |
656.10 | 61-462A-32-1,60 | 0 | 0 | 0 | ORE-ENRICHED CONCRETION | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 45 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
656.24 | 61-462A-32-1,74 | 0 | 0 | 0 | ZEOLITIC VOLCANOCLASTIC SILTSTONE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 70 | 25 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
656.66 | 61-462A-32-11,116 | 0 | 0 | 0 | ZEOLITIC VOLCANOCLASTIC SANDSTONE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 65 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
658.10 | 61-462A-32-CC,0 | 0 | 0 | 0 | ALTERED VOLCANOCLASTIC SILTSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 10 | 87 | 0 | 0 | 0 | 0 | 2 | 3 | 0 | 0 | 0 | |
663.10 | 61-462A-33-CC,0 | 0 | 0 | 0 | HIGHLY ALTERED VOLCANOCLASTIC SILTSTONEM CLAY 90/N MAINLY CHLORITE,CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
681.01 | 61-462A-35-CC,1 | 15 | 85 | 0 | VOLCANOCLASTIC SILTSTONE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 45 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | |
702.92 | 61-462A-40-1,92 | 0 | 0 | 0 | Upper aptian | ZEOLITIC CLAYSTONE | Minor lithology; relative abundance | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 88 | 10 | 0 | 1 | 0 | 0 | 2 | 2 | 0 | 0 | 0 |
703.28 | 61-462A-40-11,128 | 0 | 0 | 0 | Upper aptian | CLAYSTONE WITH PLANT REMAINS | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 10 | 78 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
703.48 | 61-462A-40-11,148 | 0 | 0 | 0 | Upper aptian | ALTERED VOLCANOCLASTIC SILTSTONE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 78 | 0 | 0 | 0 | 0 | 2 | 20 | 0 | 0 | 0 |
703.60 | 61-462A-40-2,10 | 0 | 0 | 0 | Upper aptian | CLAYSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 90 | 10 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
703.68 | 61-462A-40-2,18 | 0 | 0 | 0 | Upper aptian | ALTERED VOLCANOCLASTIC SILTSTONE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 0 | 0 | 2 | 50 | 0 | 0 | 0 |
720.36 | 61-462A-42-1,36 | 0 | 0 | 0 | ZEOLITIC VOLCANOCLASTIC SILTSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 39 | 0 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | |
720.42 | 61-462A-42-1,42 | 0 | 0 | 0 | CLAYSTONE | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | |
720.71 | 61-462A-42-1,71 | 0 | 0 | 0 | ZEOLITIC VOLCANOCLASTIC SILTSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 58 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | |
720.78 | 61-462A-42-1,78 | 0 | 0 | 0 | VOLCANOCLASTIC SILTSTONE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 0 | 0 | 2 | 50 | 0 | 0 | 0 | |
721.30 | 61-462A-41-71,130 | 0 | 0 | 0 | CLAYSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | |
721.42 | 61-462A-41-71,142 | 0 | 0 | 0 | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 94 | 0 | 0 | 0 | 1 | 2 | 0 | 0 | 5 | 0 | ||
721.59 | 61-462A-41-8,9 | 0 | 0 | 0 | CLAYSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | |
721.90 | 61-462A-41-8,40 | 0 | 0 | 0 | CLAYSTONE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 95 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
722.58 | 61-462A-42-21,108 | 0 | 0 | 0 | VOLCANOCLASTIC SILTSTONE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 0 | 0 | 2 | 0 | 2 | 40 | 0 | 0 | 0 | |
723.42 | 61-462A-43-1,42 | 0 | 0 | 0 | Lower cretaceous | VOLCANOCLASTIC SILTSTONE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 68 | 1 | 0 | 0 | 0 | 1 | 30 | 0 | 0 | 0 |
724.31 | 61-462A-43-11,131 | 0 | 0 | 0 | Lower cretaceous | VOLCANOCLASTIC SILTSTONE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 49 | 1 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 0 |
724.80 | 61-462A-43-2,30 | 0 | 0 | 0 | Lower cretaceous | VOLCANOCLASTIC SILTSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 67 | 3 | 0 | 0 | 0 | 2 | 30 | 0 | 0 | 0 |
725.97 | 61-462A-43-21,147 | 0 | 0 | 0 | Lower cretaceous | VOLCANOCLASTIC SILTSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 2 | 30 | 0 | 0 | 0 |
729.01 | 61-462A-44-1,1 | 0 | 0 | 0 | Lower cretaceous | PALAGONITE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 3 | 96 | 0 | 0 |
738.02 | 61-462A-46-1,2 | 0 | 0 | 0 | Lower cretaceous | ZEOLITIC CLAYSTONE/SILTSTONE | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 16 | 80 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
946.31 | 61-462A-X1-1,31 | 0 | 3 | 97 | Lower cretaceous | ZEOLITIC CLAYSTONE | Minor lithology; relative abundance | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 97 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 0 | 0 |
946.32 | 61-462A-X1-1,32 | 0 | 20 | 80 | Lower cretaceous | ZEOLITIC MUDSTONE ( TO SHALE) | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 83 | 0 | 0 | 0 | 2 | 0 | 2 | 10 | 1 | 2 | 0 |
946.33 | 61-462A-X1-1,33 | 0 | 30 | 70 | Lower cretaceous | ZEOLITIC MUDSTONE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 40 | 0 | 0 | 0 | 0 | 0 | 2 | 15 | 45 | 0 | 0 |
946.34 | 61-462A-X1-1,34 | 0 | 50 | 50 | Lower cretaceous | NANNOFOSSIL CHALK | Minor lithology; numerical abundance | 18 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 0 | 0 |
992.57 | 61-462A-79-6,7 | 0 | 0 | 0 | Lower cretaceous | (DEVITRIFIED VOLCANIC ASH) CLAYSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 55 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
992.62 | 61-462A-79-6,12 | 0 | 0 | 0 | Lower cretaceous | CLAYSTONE (DEVITRIFIED VOLCANIC ASH) | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 75 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |