Hsü, Kenneth J; Montadert, Lucien; Ross, David A (2005): Smear slide analysis of Hole 42-380A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230716
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
Worstell, Paula J; Mélières, Frédéric; Bernoulli, Daniel; Erickson, A J; Wright, Ramil; Bizon, G; Cita, Maria Bianca; Müller, Carla; Kidd, Robert B; Fabricius, F H; Garrison, Robert E; Hsü, Kenneth J; Montadert, Lucien (1978): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XLII Pt. 1, 1249 pp + 1244 pp, https://doi.org/10.2973/dsdp.proc.42-1.1978
Further details:
Processed smear slide data base - background and methods. hdl:10013/epic.32353.d001
Project(s):
Funding:
Sixth Framework Programme (FP6), grant/award no. 36949: Southern European Seas: Assessing and Modelling Ecosystem Changes
Coverage:
Latitude: 42.099000 * Longitude: 29.613700
Date/Time Start: 1975-05-30T00:00:00 * Date/Time End: 1975-05-30T00:00:00
Minimum DEPTH, sediment/rock: 333.87 m * Maximum DEPTH, sediment/rock: 1074.75 m
Event(s):
42-380A * Latitude: 42.099000 * Longitude: 29.613700 * Date/Time: 1975-05-30T00:00:00 * Elevation: -2107.0 m * Penetration: 1083 m * Recovery: 422 m * Location: Black Sea * Campaign: Leg42 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 78 cores; 727.5 m cored; 19 m drilled; 58 % 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 | Aragonite | Arg | % | Smear slide analysis | ||
12 | Nannofossils | Nannos | % | Smear slide analysis | ||
13 | Foraminifera | Foram | % | Smear slide analysis | ||
14 | Diatoms | Diatoms | % | Smear slide analysis | ||
15 | Siderite | Sd | % | 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 | Heavy minerals | HM | % | Smear slide analysis | ||
25 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
26 | Organic matter | OM | % | Smear slide analysis | organic debris |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
5224 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 Arg [%] | 12 Nannos [%] | 13 Foram [%] | 14 Diatoms [%] | 15 Sd [%] | 16 Qz [%] | 17 Fsp [%] | 18 Zeo [%] | 19 Mica [%] | 20 Clay min [%] | 21 Glt [%] | 22 Opaque [%] | 23 Py [%] | 24 HM [%] | 25 Volc glass [%] | 26 OM [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
333.87 | 42-380A-1-11,137 | 0 | 65 | 35 | Pleistocene | PYRITE RICH MUD | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 35 | 0 | 0 | 15 | 6 | 0 | 0 |
334.88 | 42-380A-1-2,88 | 0 | 25 | 75 | Pleistocene | ORGANIC RICH MUD | Dominat lithology; relative abundance | 5 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 6 | 75 | 0 | 0 | 10 | 0 | 0 | 0 |
336.75 | 42-380A-1-31,125 | 0 | 30 | 70 | Pleistocene | MUD | Dominat lithology; numerical abundance | 10 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 65 | 0 | 0 | 2 | 1 | 0 | 0 |
350.95 | 42-380A-2-61,105 | 0 | 10 | 90 | Pleistocene | DOLOMITE MARL | Minor lithology; numerical abundance | 4 | 45 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 1 | 0 | 0 | 0 |
351.04 | 42-380A-2-61,114 | 0 | 15 | 85 | Pleistocene | MUD | Dominat lithology; relative abundance | 8 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 85 | 0 | 0 | 2 | 0 | 0 | 0 |
357.40 | 42-380A-3-41,140 | 0 | 70 | 30 | Pleistocene | DIATOM MUD | Dominat lithology; relative abundance | 3 | 0 | 0 | 6 | 0 | 50 | 0 | 0 | 0 | 0 | 1 | 30 | 0 | 0 | 10 | 1 | 0 | 0 |
357.42 | 42-380A-3-41,142 | 0 | 80 | 20 | Pleistocene | DIATOM OOZE | Minor lithology; relative abundance | 4 | 0 | 0 | 6 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 1 | 0 | 0 | 0 |
361.37 | 42-380A-4-1,37 | 0 | 20 | 80 | Pleistocene | CLAY | Dominat lithology; numerical abundance | 4 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 0 |
361.39 | 42-380A-4-1,39 | 0 | 25 | 75 | Pleistocene | MUD | Dominat lithology; numerical abundance | 5 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 75 | 0 | 0 | 2 | 0 | 0 | 0 |
363.60 | 42-380A-4-21,110 | 0 | 15 | 85 | Pleistocene | MUD | Dominat lithology; numerical abundance | 3 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 85 | 0 | 0 | 0 | 0 | 0 | 0 |
365.30 | 42-380A-4-31,130 | 0 | 15 | 85 | Pleistocene | NANNO OOZE | Minor lithology; numerical abundance | 5 | 0 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 35 | 0 | 0 | 0 | 0 | 0 | 0 |
365.31 | 42-380A-4-31,130.5 | 0 | 10 | 85 | Pleistocene | CLAY | Dominat lithology; numerical abundance | 5 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 85 | 0 | 0 | 2 | 0 | 0 | 0 |
365.31 | 42-380A-4-31,130.5 | 0 | 15 | 90 | Pleistocene | SILTY CLAY | Dominat lithology; relative abundance | 6 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 90 | 0 | 0 | 3 | 0 | 0 | 0 |
365.72 | 42-380A-4-4,22 | 0 | 0 | 0 | Pleistocene | DOLOMITE | Minor lithology; numerical abundance | 1 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
370.94 | 42-380A-5-1,44 | 0 | 20 | 80 | Pleistocene | MUD | Minor lithology; numerical abundance | 10 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 75 | 0 | 0 | 2 | 0 | 0 | 0 |
374.20 | 42-380A-5-3,70 | 0 | 30 | 70 | Pleistocene | MUD | Dominat lithology; numerical abundance | 15 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 70 | 0 | 0 | 2 | 1 | 0 | 0 |
377.75 | 42-380A-5-51,125 | 0 | 65 | 35 | Pleistocene | MUD | Minor lithology; numerical abundance | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 18 | 35 | 0 | 0 | 4 | 2 | 0 | 0 |
377.80 | 42-380A-5-51,129.5 | 0 | 20 | 80 | Pleistocene | PYRITE RICH CLAY | Minor lithology; relative abundance | 6 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 0 | 15 | 0 | 0 | 0 |
381.23 | 42-380A-6-11,123 | 0 | 30 | 70 | Pleistocene | ORGANIC RICH MUD | Dominat lithology; relative abundance | 5 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 70 | 0 | 0 | 10 | 0 | 0 | 0 |
381.25 | 42-380A-6-11,125 | 0 | 60 | 40 | Pleistocene | MUD | Dominat lithology; relative abundance | 10 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 |
381.34 | 42-380A-6-11,134 | 30 | 30 | 40 | Pleistocene | PYRITE RICH SANDY MUD | Minor lithology; numerical abundance | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 15 | 0 | 0 | 0 |
381.44 | 42-380A-6-11,144 | 0 | 95 | 5 | Pleistocene | SILT | Dominat lithology; numerical abundance | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 5 | 1 | 0 | 2 | 2 | 0 | 0 |
383.75 | 42-380A-6-3,75 | 0 | 10 | 90 | Pleistocene | DOLOMITE MARL | Minor lithology; numerical abundance | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
383.78 | 42-380A-6-3,78 | 0 | 40 | 60 | Pleistocene | PYRITE RICH MUD | Dominat lithology; relative abundance | 5 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 0 | 0 | 20 | 0 | 0 | 0 |
383.92 | 42-380A-6-3,92 | 0 | 60 | 40 | Pleistocene | MUD | Dominat lithology; numerical abundance | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 3 | 0 | 0 | 0 |
383.92 | 42-380A-6-3,92 | 0 | 60 | 40 | Pleistocene | MUD | Dominat lithology; numerical abundance | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 3 | 0 | 0 | 0 |
384.58 | 42-380A-6-4,8 | 0 | 60 | 40 | Pleistocene | PYRITE RICH MUD | Minor lithology; numerical abundance | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 30 | 0 | 0 | 0 |
401.53 | 42-380A-8-2,63 | 0 | 10 | 90 | Pleistocene | CLAY | Minor lithology; relative abundance | 3 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 90 | 0 | 0 | 3 | 0 | 0 | 0 |
401.56 | 42-380A-8-2,66 | 0 | 30 | 70 | Pleistocene | MUD | Dominat lithology; relative abundance | 10 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 70 | 0 | 0 | 1 | 6 | 0 | 0 |
401.95 | 42-380A-8-21,105 | 0 | 15 | 85 | Pleistocene | MUD | Dominat lithology; numerical abundance | 5 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 85 | 0 | 0 | 4 | 0 | 0 | 0 |
402.00 | 42-380A-8-21,110 | 0 | 15 | 85 | Pleistocene | DOLOMITE MARL | Minor lithology; relative abundance | 5 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
404.50 | 42-380A-8-4,60 | 0 | 10 | 90 | Pleistocene | CLAY | Dominat lithology; numerical abundance | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 75 | 0 | 0 | 2 | 0 | 0 | 15 |
406.90 | 42-380A-8-51,150 | 0 | 0 | 0 | Pleistocene | DOLOMITE MARL | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
409.70 | 42-380A-9-11,120 | 0 | 0 | 0 | Pleistocene | ORGANIC RICH CLAY | Dominat lithology; relative abundance | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 90 | 0 | 0 | 4 | 0 | 0 | 0 |
409.78 | 42-380A-9-11,128 | 0 | 0 | 0 | Pleistocene | DOLOMITE MARL | Minor lithology; numerical abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 |
412.80 | 42-380A-9-31,130 | 0 | 25 | 75 | Pleistocene | MUD | Dominat lithology; relative abundance | 6 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 75 | 0 | 0 | 2 | 6 | 0 | 0 |
412.85 | 42-380A-9-31,135 | 0 | 0 | 0 | Pleistocene | DOLOMITE MARL | Dominat lithology; relative abundance | 14 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 |
412.88 | 42-380A-9-31,138 | 20 | 70 | 10 | Pleistocene | SANDY SILT | Minor lithology; relative abundance | 20 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 10 | 0 | 0 | 1 | 1 | 0 | 0 |
416.99 | 42-380A-9-6,99 | 0 | 60 | 40 | Pleistocene | DOLOMITE MARL | Minor lithology; numerical abundance | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 |
417.00 | 42-380A-9-61,100 | 0 | 80 | 20 | Pleistocene | MICRITE | Dominat lithology; relative abundance | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 20 | 0 | 0 | 6 | 0 | 0 | 0 |
418.41 | 42-380A-10-1,41 | 0 | 85 | 15 | Pleistocene | MICRITE | Dominat lithology; relative abundance | 85 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 6 | 0 | 0 | 0 |
418.52 | 42-380A-10-1,52 | 0 | 0 | 0 | Pleistocene | MARL | Dominat lithology; relative abundance | 50 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 6 | 0 | 0 | 0 |
418.55 | 42-380A-10-1,55 | 40 | 40 | 20 | Pleistocene | SANDY MUD | Minor lithology; relative abundance | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 6 | 0 | 0 | 0 |
419.50 | 42-380A-10-11,150 | 0 | 10 | 90 | Pleistocene | MICRITE | Dominat lithology; numerical abundance | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 |
428.85 | 42-380A-11-11,135 | 0 | 70 | 30 | Pleistocene | SILTY MUD | Dominat lithology; numerical abundance | 45 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 5 | 0 | 0 | 0 |
429.78 | 42-380A-11-2,78 | 0 | 50 | 50 | Pleistocene | MUD | Dominat lithology; numerical abundance | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 10 | 0 | 0 | 0 |
429.98 | 42-380A-11-2,98 | 0 | 50 | 50 | Pleistocene | PYRITE RICH MUD | Dominat lithology; numerical abundance | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 15 | 0 | 0 | 0 |
439.83 | 42-380A-12-2,95 | 0 | 0 | 0 | Pleistocene | MUD | Dominat lithology; numerical abundance | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 0 | 0 | 5 | 0 | 0 | 0 |
440.98 | 42-380A-12-3,60 | 0 | 40 | 60 | Pleistocene | PYRITE RICH MUD | Minor lithology; numerical abundance | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 0 | 0 | 15 | 0 | 0 | 0 |
442.61 | 42-380A-12-4,73 | 0 | 90 | 10 | Pleistocene | MICRITE | Dominat lithology; numerical abundance | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 0 | 2 | 0 | 0 | 0 |
458.92 | 42-380A-14-21,142 | 0 | 0 | 0 | Pleistocene | MICRITE | Dominat lithology; relative abundance | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 10 | 0 | 0 | 6 | 0 | 0 | 0 |
459.47 | 42-380A-14-3,47 | 0 | 75 | 25 | Pleistocene | MARL | Dominat lithology; numerical abundance | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 0 | 0 | 0 | 0 | 0 |
459.49 | 42-380A-14-3,49 | 0 | 0 | 0 | Pleistocene | MICRITE | Dominat lithology; relative abundance | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 6 | 0 | 0 | 0 | 0 |
467.54 | 42-380A-15-2,54 | 0 | 35 | 65 | Pleistocene | MUD | Dominat lithology; numerical abundance | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 65 | 0 | 0 | 10 | 0 | 0 | 0 |
467.56 | 42-380A-15-2,56 | 0 | 50 | 50 | Pleistocene | LAKE MARL | Dominat lithology; relative abundance | 35 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 6 | 0 | 0 | 0 |
468.25 | 42-380A-15-21,125 | 0 | 0 | 0 | Pleistocene | PYRITE RICH MUD | Minor lithology; relative abundance | 35 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
472.65 | 42-380A-15-51,115 | 0 | 50 | 50 | Pleistocene | MARL | Dominat lithology; relative abundance | 35 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 2 | 0 | 0 | 0 |
475.55 | 42-380A-16-1,55 | 0 | 60 | 40 | Pleistocene | LAKE MARL | Dominat lithology; numerical abundance | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 |
476.15 | 42-380A-16-11,115 | 0 | 10 | 90 | Pleistocene | ORGANIC RICH CLAY | Dominat lithology; relative abundance | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 90 | 0 | 0 | 7 | 0 | 0 | 0 |
485.40 | 42-380A-17-1,50 | 0 | 55 | 45 | Pleistocene | DIATOM MUD | Minor lithology; relative abundance | 6 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 45 | 0 | 0 | 5 | 6 | 0 | 0 |
485.79 | 42-380A-17-1,89 | 0 | 0 | 0 | Pleistocene | DIATOM MARL | Dominat lithology; numerical abundance | 40 | 0 | 0 | 0 | 0 | 25 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 3 | 0 | 0 | 0 |
486.88 | 42-380A-17-2,48 | 0 | 0 | 0 | Pleistocene | MICRITE | Dominat lithology; numerical abundance | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 2 | 0 | 0 | 0 |
486.90 | 42-380A-17-2,50 | 0 | 0 | 0 | Pleistocene | MARL | Dominat lithology; relative abundance | 80 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 2 | 0 | 0 | 0 |
487.80 | 42-380A-17-21,140 | 0 | 0 | 0 | Pleistocene | MUD | Dominat lithology; relative abundance | 6 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 5 | 80 | 0 | 0 | 10 | 0 | 0 | 0 |
490.54 | 42-380A-17-41,114 | 0 | 55 | 45 | Pleistocene | MUD | Dominat lithology; relative abundance | 30 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 45 | 0 | 0 | 10 | 0 | 0 | 0 |
490.58 | 42-380A-17-41,118 | 0 | 0 | 0 | Pleistocene | MICRITE | Dominat lithology; relative abundance | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 6 | 0 | 0 | 0 |
496.77 | 42-380A-18-21,127 | 0 | 20 | 80 | Pleistocene | MUD | Dominat lithology; relative abundance | 5 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 0 | 5 | 0 | 0 | 0 |
496.97 | 42-380A-18-21,147 | 0 | 0 | 0 | Pleistocene | MICRITE | Minor lithology; relative abundance | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 6 | 0 | 0 | 0 |
509.45 | 42-380A-19-41,110 | 0 | 55 | 45 | Pleistocene | MUD | Dominat lithology; numerical abundance | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 45 | 0 | 0 | 10 | 0 | 0 | 0 |
509.76 | 42-380A-19-41,141 | 0 | 90 | 10 | Pleistocene | MICRITE | Dominat lithology; relative abundance | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 6 | 0 | 0 | 0 |
514.69 | 42-380A-20-2,19 | 0 | 50 | 50 | Pleistocene | PYRITE RICH MUD | Minor lithology; relative abundance | 20 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 20 | 0 | 0 | 0 |
514.71 | 42-380A-20-2,21 | 0 | 55 | 45 | Pleistocene | MARL | Dominat lithology; relative abundance | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 45 | 0 | 0 | 6 | 0 | 0 | 0 |
514.77 | 42-380A-20-2,27 | 0 | 50 | 50 | Pleistocene | MARL | Minor lithology; relative abundance | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 6 | 0 | 0 | 0 |
516.10 | 42-380A-20-3,10 | 0 | 60 | 40 | Pleistocene | MARL | Dominat lithology; relative abundance | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 6 | 0 | 0 | 0 |
523.68 | 42-380A-21-11,118 | 0 | 25 | 75 | Pleistocene | MUD | Dominat lithology; numerical abundance | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 75 | 0 | 0 | 5 | 0 | 0 | 0 |
523.74 | 42-380A-21-11,124 | 0 | 60 | 35 | Pleistocene | MARL | Dominat lithology; relative abundance | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 35 | 0 | 0 | 6 | 0 | 0 | 0 |
535.40 | 42-380A-22-3,40 | 0 | 20 | 80 | Pleistocene | MUD | Dominat lithology; numerical abundance | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 0 | 5 | 0 | 0 | 0 |
535.90 | 42-380A-22-3,90 | 0 | 0 | 0 | Pleistocene | MICRITE | Dominat lithology; numerical abundance | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 2 | 0 | 0 | 0 |
538.96 | 42-380A-22-5,96 | 0 | 0 | 0 | Pleistocene | MARL | Dominat lithology; numerical abundance | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 5 | 0 | 0 | 0 |
538.98 | 42-380A-22-5,98 | 0 | 90 | 10 | Pleistocene | MICRITE | Dominat lithology; relative abundance | 85 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 6 | 0 | 0 | 0 |
539.84 | 42-380A-22-6,34 | 0 | 55 | 45 | Pleistocene | MUD | Dominat lithology; numerical abundance | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 45 | 0 | 0 | 5 | 0 | 0 | 0 |
540.95 | 42-380A-22-61,145 | 0 | 90 | 10 | Pleistocene | MICRITE | Dominat lithology; numerical abundance | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 |
562.37 | 42-380A-25-2,37 | 0 | 20 | 80 | Pleistocene | ORGANIC RICH MUD | Dominat lithology; relative abundance | 3 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 0 | 10 | 0 | 0 | 0 |
562.45 | 42-380A-25-2,45 | 0 | 90 | 10 | Pleistocene | MICRITE | Minor lithology; numerical abundance | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 5 | 0 | 0 | 0 |
562.46 | 42-380A-25-2,46 | 0 | 45 | 55 | Pleistocene | ORGANIC RICH MUD | Dominat lithology; relative abundance | 25 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 10 | 0 | 0 | 0 |
563.76 | 42-380A-25-3,26 | 0 | 20 | 80 | Pleistocene | MUD | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 80 | 6 | 0 | 8 | 0 | 0 | 0 |
571.10 | 42-380A-26-11,110 | 0 | 90 | 10 | Pleistocene | MICRITE | Dominat lithology; numerical abundance | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 1 | 0 | 0 | 0 |
571.34 | 42-380A-26-11,134 | 0 | 50 | 50 | Pleistocene | MARL | Dominat lithology; numerical abundance | 35 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 2 | 0 | 0 | 0 |
582.74 | 42-380A-27-3,24 | 0 | 10 | 90 | Pleistocene | MUD | Dominat lithology; numerical abundance | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 85 | 0 | 0 | 5 | 0 | 0 | 0 |
582.85 | 42-380A-27-3,35 | 0 | 0 | 0 | Pleistocene | MICRITE | Dominat lithology; relative abundance | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 6 | 0 | 0 | 0 |
593.09 | 42-380A-29-1,9 | 0 | 20 | 80 | Pleistocene | MUD | Dominat lithology; numerical abundance | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 75 | 0 | 0 | 10 | 0 | 0 | 0 |
594.45 | 42-380A-29-11,145 | 0 | 85 | 15 | Pleistocene | MICRITE | Dominat lithology; relative abundance | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 15 | 0 | 0 | 6 | 0 | 0 | 0 |
595.90 | 42-380A-29-21,140 | 0 | 0 | 0 | Pleistocene | MICRITE | Dominat lithology; numerical abundance | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 |
599.64 | 42-380A-30-11,114 | 0 | 90 | 10 | Pleistocene | SILT | Minor lithology; numerical abundance | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 10 | 0 | 0 | 6 | 2 | 0 | 0 |
601.50 | 42-380A-29-61,100 | 0 | 0 | 0 | Pleistocene | MICRITE | Dominat lithology; numerical abundance | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 2 | 0 | 0 | 0 |
608.32 | 42-380A-31-1,32 | 0 | 20 | 80 | Pleistocene | MUD | Dominat lithology; numerical abundance | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 0 | 5 | 0 | 0 | 0 |
608.80 | 42-380A-31-1,80 | 0 | 20 | 80 | Pleistocene | MUD | Dominat lithology; numerical abundance | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 0 | 10 | 0 | 0 | 0 |
609.45 | 42-380A-31-11,145 | 0 | 70 | 30 | Pleistocene | MARL | Dominat lithology; relative abundance | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 6 | 0 | 0 | 0 |
613.06 | 42-380A-31-4,56 | 0 | 95 | 5 | Pleistocene | MICRITE | Minor lithology; numerical abundance | 85 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 1 | 0 | 0 | 0 |
623.35 | 42-380A-32-41,100 | 0 | 50 | 50 | Pleistocene | MARL | Dominat lithology; numerical abundance | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 0 |
625.50 | 42-380A-32-6,15 | 0 | 0 | 0 | Pleistocene | MICRITE | Dominat lithology; relative abundance | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 6 | 0 | 0 | 0 |
625.60 | 42-380A-32-6,25 | 0 | 0 | 0 | Pleistocene | MICRITE | Dominat lithology; relative abundance | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 6 | 0 | 0 | 0 |
634.27 | 42-380A-33-3,27 | 0 | 0 | 0 | Pleistocene | PYRITE | Minor lithology; numerical abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 90 | 0 | 0 | 0 |
640.10 | 42-380A-34-3,60 | 0 | 45 | 55 | Pleistocene | MARL | Dominat lithology; numerical abundance | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 |
643.54 | 42-380A-34-51,104 | 0 | 35 | 65 | Pleistocene | MARL | Dominat lithology; relative abundance | 35 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 45 | 0 | 0 | 6 | 0 | 0 | 0 |
643.78 | 42-380A-34-51,128 | 0 | 10 | 90 | Pleistocene | CLAY | Dominat lithology; relative abundance | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 90 | 0 | 0 | 5 | 0 | 0 | 0 |
649.92 | 42-380A-35-3,92 | 0 | 10 | 90 | Pleistocene | CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 3 | 0 | 0 | 90 | 0 | 0 | 2 | 0 | 0 | 0 |
656.40 | 42-380A-36-1,90 | 0 | 5 | 95 | Pleistocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 95 | 0 | 0 | 6 | 0 | 0 | 0 |
657.79 | 42-380A-36-2,79 | 0 | 0 | 0 | Pleistocene | SIDERITE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 |
659.30 | 42-380A-36-3,80 | 0 | 10 | 90 | Pleistocene | CLAY | Dominat lithology; relative abundance | 6 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 90 | 0 | 0 | 2 | 0 | 0 | 0 |
668.90 | 42-380A-37-3,90 | 0 | 5 | 95 | Pleistocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 95 | 0 | 0 | 6 | 0 | 0 | 0 |
670.40 | 42-380A-37-4,90 | 0 | 0 | 0 | Pleistocene | DIATOM RICH MUD | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 0 | 6 | 0 | 0 | 0 |
675.60 | 42-380A-38-1,75 | 0 | 10 | 90 | Pleistocene | PYRITE RICH CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 85 | 0 | 0 | 10 | 0 | 0 | 0 |
679.23 | 42-380A-38-31,138 | 0 | 0 | 0 | Pleistocene | DIATOMACEOUS CLAY | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 5 | 0 | 0 | 0 |
681.85 | 42-380A-38-51,100 | 0 | 15 | 85 | Pleistocene | DIATOM RICH CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 75 | 0 | 0 | 5 | 0 | 0 | 0 |
688.01 | 42-380A-39-31,101 | 0 | 0 | 0 | Pleistocene | DIATOMACEOUS CLAY | Dominat lithology; relative abundance | 6 | 0 | 0 | 0 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 6 | 0 | 0 | 0 |
688.02 | 42-380A-39-31,102 | 0 | 70 | 30 | Pleistocene | CLAYEY DIATOM OOZE | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 5 | 0 | 0 | 0 |
698.96 | 42-380A-40-4,96 | 0 | 5 | 95 | Pleistocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 95 | 0 | 0 | 6 | 0 | 0 | 0 |
705.40 | 42-380A-41-2,60 | 0 | 6 | 5 | Pleistocene | CLAYEY DIATOM OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 65 | 0 | 0 | 0 | 0 | 0 | 35 | 0 | 0 | 1 | 0 | 0 | 0 |
708.30 | 42-380A-41-4,50 | 0 | 20 | 80 | Pleistocene | DIATOM RICH CLAY | Dominat lithology; relative abundance | 6 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 0 | 6 | 0 | 0 | 0 |
708.41 | 42-380A-41-4,61 | 0 | 0 | 0 | Pleistocene | SIDERITE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 10 | 70 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 6 | 0 | 0 | 0 |
710.71 | 42-380A-41-51,141 | 0 | 15 | 20 | Pleistocene | CLAYEY DIATOM OOZE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 6 | 0 | 0 | 0 |
710.71 | 42-380A-41-51,141 | 0 | 80 | 85 | Pleistocene | DIATOM RICH CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 85 | 0 | 0 | 6 | 0 | 0 | 0 |
712.75 | 42-380A-42-1,5 | 0 | 0 | 0 | Pleistocene | SIDERITE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 6 | 0 | 0 | 0 |
713.60 | 42-380A-42-1,90 | 0 | 35 | 65 | Pleistocene | DIATOM RICH CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 65 | 0 | 0 | 5 | 0 | 0 | 0 |
717.60 | 42-380A-42-4,40 | 0 | 90 | 10 | Pleistocene | CARBONATE | Dominat lithology; relative abundance | 80 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 6 | 0 | 0 | 0 |
717.93 | 42-380A-42-4,73 | 0 | 45 | 55 | Pleistocene | DIATOM RICH CLAY | Dominat lithology; numerical abundance | 5 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 5 | 0 | 0 | 0 |
721.13 | 42-380A-42-6,93 | 0 | 50 | 50 | Pleistocene | DIATOMACEOUS CLAY | Dominat lithology; relative abundance | 10 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 6 | 0 | 0 | 0 |
724.70 | 42-380A-43-2,80 | 0 | 50 | 50 | Pleistocene | MARL | Dominat lithology; relative abundance | 30 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 6 | 50 | 0 | 0 | 6 | 0 | 0 | 0 |
724.71 | 42-380A-43-2,81 | 0 | 10 | 90 | Pleistocene | CLAY | Dominat lithology; relative abundance | 6 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 90 | 0 | 0 | 2 | 0 | 0 | 0 |
727.46 | 42-380A-43-4,56 | 0 | 55 | 45 | Pleistocene | MARL | Dominat lithology; relative abundance | 30 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 45 | 0 | 0 | 6 | 0 | 0 | 0 |
733.26 | 42-380A-44-2,26 | 0 | 0 | 0 | Pleistocene | MARL | Dominat lithology; relative abundance | 20 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 6 | 0 | 0 | 0 |
733.68 | 42-380A-44-2,68 | 0 | 50 | 50 | Pleistocene | DIATOMACEOUS CLAY | Minor lithology; relative abundance | 6 | 0 | 0 | 0 | 0 | 45 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 1 | 0 | 0 | 0 |
733.69 | 42-380A-44-2,69 | 0 | 30 | 70 | Pleistocene | DIATOM RICH CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 70 | 0 | 0 | 6 | 0 | 0 | 0 |
766.50 | 42-380A-47-5,50 | 0 | 70 | 30 | Pleistocene | MARL | Dominat lithology; numerical abundance | 40 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 1 | 0 | 0 | 0 |
767.37 | 42-380A-47-51,137 | 0 | 60 | 40 | Pleistocene | MARL | Dominat lithology; numerical abundance | 30 | 0 | 0 | 0 | 0 | 7 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 3 | 0 | 0 | 0 |
774.70 | 42-380A-48-4,35 | 0 | 0 | 0 | Pleistocene | MARL | Minor lithology; relative abundance | 25 | 0 | 0 | 6 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 10 | 0 | 0 | 0 |
774.71 | 42-380A-48-4,36 | 0 | 5 | 95 | Pleistocene | CLAY | Minor lithology; relative abundance | 6 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 95 | 0 | 0 | 2 | 0 | 0 | 0 |
775.80 | 42-380A-48-41,145 | 0 | 55 | 45 | Pleistocene | MARL | Dominat lithology; relative abundance | 35 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 45 | 0 | 0 | 6 | 0 | 0 | 0 |
778.83 | 42-380A-48-61,148 | 0 | 0 | 0 | Pleistocene | MARL | Minor lithology; relative abundance | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 6 | 0 | 0 | 0 |
779.77 | 42-380A-49-1,77 | 0 | 60 | 40 | Pleistocene | MARL | Minor lithology; relative abundance | 35 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 5 | 6 | 0 | 0 |
779.80 | 42-380A-49-1,80 | 0 | 55 | 45 | Pleistocene | MARL | Minor lithology; relative abundance | 55 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 45 | 0 | 0 | 6 | 0 | 0 | 0 |
784.33 | 42-380A-49-4,83 | 0 | 55 | 45 | Pleistocene | DIATOM RICH MARL | Dominat lithology; relative abundance | 30 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 45 | 0 | 0 | 1 | 6 | 0 | 0 |
784.49 | 42-380A-49-4,99 | 0 | 10 | 90 | Pleistocene | CLAY | Minor lithology; numerical abundance | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 90 | 0 | 0 | 2 | 0 | 0 | 0 |
785.93 | 42-380A-49-5,93 | 0 | 55 | 45 | Pleistocene | MARL | Dominat lithology; relative abundance | 30 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 45 | 0 | 0 | 5 | 6 | 0 | 0 |
785.96 | 42-380A-49-5,96 | 0 | 0 | 0 | Pleistocene | MICRITE | Minor lithology; relative abundance | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 6 | 0 | 0 | 0 |
789.83 | 42-380A-50-11,133 | 0 | 90 | 10 | Pleistocene | MICRITE | Minor lithology; relative abundance | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 10 | 0 | 0 | 8 | 0 | 0 | 0 |
790.14 | 42-380A-50-2,14 | 0 | 90 | 10 | Pleistocene | MICRITE | Minor lithology; relative abundance | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 6 | 0 | 0 | 0 |
790.15 | 42-380A-50-2,15 | 0 | 0 | 0 | Pleistocene | PYRITE RICH CLAY | Minor lithology; relative abundance | 6 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 0 | 15 | 0 | 0 | 0 |
790.20 | 42-380A-50-2,20 | 0 | 45 | 55 | Pleistocene | DIATOM RICH CLAY | Dominat lithology; relative abundance | 20 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 6 | 0 | 0 | 0 |
790.28 | 42-380A-50-2,28 | 0 | 55 | 45 | Pleistocene | MARL | Dominat lithology; relative abundance | 45 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 45 | 0 | 0 | 6 | 0 | 0 | 0 |
798.93 | 42-380A-51-1,53 | 0 | 60 | 40 | Pleistocene | MARL | Dominat lithology; numerical abundance | 40 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 2 | 0 | 0 | 0 |
799.13 | 42-380A-51-1,73 | 0 | 90 | 10 | Pleistocene | MICRITE | Minor lithology; relative abundance | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 6 | 0 | 0 | 0 |
802.16 | 42-380A-51-3,76 | 0 | 0 | 0 | Pleistocene | MICRITE | Minor lithology; relative abundance | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 6 | 0 | 0 | 0 |
806.75 | 42-380A-51-6,85 | 0 | 55 | 45 | Pleistocene | DIATOM RICH MUD | Dominat lithology; relative abundance | 40 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 45 | 0 | 0 | 6 | 6 | 0 | 0 |
809.65 | 42-380A-52-2,30 | 0 | 0 | 0 | Pleistocene | MICRITE | Dominat lithology; relative abundance | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 0 | 6 | 0 | 0 | 0 |
809.77 | 42-380A-52-2,42 | 0 | 60 | 40 | Pleistocene | MARL | Dominat lithology; numerical abundance | 45 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 5 | 0 | 0 | 0 |
815.39 | 42-380A-52-6,4 | 5 | 75 | 20 | Pleistocene | SILT | Minor lithology; relative abundance | 25 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 6 | 20 | 0 | 0 | 5 | 6 | 0 | 0 |
815.40 | 42-380A-52-6,4.5 | 0 | 0 | 0 | Pleistocene | MICRITE | Minor lithology; relative abundance | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 6 | 0 | 0 | 0 |
818.16 | 42-380A-53-11,116 | 0 | 50 | 50 | Pleistocene | MARL | Dominat lithology; relative abundance | 35 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 6 | 50 | 0 | 0 | 2 | 0 | 0 | 0 |
819.43 | 42-380A-53-2,93 | 0 | 0 | 0 | Pleistocene | MICRITE | Dominat lithology; relative abundance | 85 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 6 | 0 | 0 | 0 |
820.54 | 42-380A-53-3,54 | 0 | 55 | 45 | Pleistocene | MARL | Dominat lithology; relative abundance | 40 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 6 | 45 | 0 | 0 | 6 | 0 | 0 | 0 |
826.55 | 42-380A-54-1,5 | 0 | 30 | 70 | Pleistocene | DIATOM RICH CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 6 | 70 | 0 | 0 | 6 | 0 | 0 | 0 |
839.30 | 42-380A-55-3,30 | 0 | 0 | 0 | Pleistocene | DIATOM RICH MUD | Dominat lithology; relative abundance | 6 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 6 | 65 | 0 | 0 | 5 | 0 | 0 | 0 |
841.33 | 42-380A-55-4,83 | 0 | 0 | 0 | Pleistocene | DIATOM RICH MUD | Dominat lithology; relative abundance | 6 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 6 | 75 | 0 | 0 | 5 | 0 | 0 | 0 |
848.90 | 42-380A-56-3,40 | 0 | 30 | 70 | Pleistocene | DIATOM RICH CLAY | Dominat lithology; relative abundance | 6 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 6 | 70 | 0 | 0 | 15 | 6 | 0 | 0 |
850.37 | 42-380A-56-4,37 | 0 | 0 | 0 | Pleistocene | DIATOM BEARING MUDSTONE | Dominat lithology; relative abundance | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 6 | 0 | 0 | 0 |
850.46 | 42-380A-56-4,46 | 0 | 0 | 0 | Pleistocene | MICRITE | Minor lithology; numerical abundance | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
850.81 | 42-380A-56-4,81 | 0 | 0 | 0 | Pleistocene | MARL | Dominat lithology; relative abundance | 20 | 0 | 0 | 5 | 0 | 10 | 0 | 0 | 0 | 0 | 6 | 50 | 0 | 0 | 10 | 0 | 0 | 0 |
855.65 | 42-380A-57-1,65 | 0 | 0 | 0 | Pleistocene | MARL | Dominat lithology; relative abundance | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 30 | 0 | 0 | 6 | 0 | 0 | 0 |
855.85 | 42-380A-57-1,85 | 50 | 30 | 20 | Pleistocene | SILTY SAND | Dominat lithology; relative abundance | 30 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 20 | 0 | 0 | 6 | 0 | 0 | 0 |
863.55 | 42-380A-57-61,105 | 0 | 40 | 60 | Pleistocene | MARL | Minor lithology; relative abundance | 15 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 65 | 0 | 0 | 10 | 0 | 0 | 0 |
868.05 | 42-380A-58-3,55 | 0 | 0 | 0 | Pleistocene | MARL | Dominat lithology; relative abundance | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 30 | 0 | 0 | 0 | 6 | 0 | 0 |
883.85 | 42-380A-60-1,35 | 0 | 0 | 0 | Pleistocene | MARL | Dominat lithology; relative abundance | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 40 | 0 | 0 | 5 | 0 | 0 | 0 |
883.86 | 42-380A-60-1,36 | 0 | 15 | 85 | Pleistocene | CLAY | Minor lithology; numerical abundance | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 85 | 0 | 0 | 5 | 0 | 0 | 0 |
887.47 | 42-380A-60-3,97 | 0 | 0 | 0 | Pleistocene | MARL | Dominat lithology; numerical abundance | 35 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 5 | 0 | 0 | 0 |
904.50 | 42-380A-62-2,50 | 0 | 0 | 0 | Pleistocene | MARL | Dominat lithology; numerical abundance | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 2 | 0 | 0 | 0 |
904.52 | 42-380A-62-2,52 | 0 | 0 | 0 | Pleistocene | MUD | Minor lithology; numerical abundance | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 60 | 0 | 0 | 8 | 0 | 0 | 0 |
916.19 | 42-380A-63-31,119 | 0 | 0 | 0 | Pleistocene | DOLOMITE | Minor lithology; numerical abundance | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
916.54 | 42-380A-63-4,4 | 0 | 0 | 0 | Pleistocene | ARAGONITE | Minor lithology; relative abundance | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 |
923.28 | 42-380A-64-2,28 | 0 | 15 | 85 | Pleistocene | CLAY | Dominat lithology; relative abundance | 6 | 0 | 0 | 6 | 0 | 6 | 0 | 0 | 0 | 0 | 2 | 85 | 0 | 0 | 8 | 0 | 0 | 0 |
926.93 | 42-380A-64-4,93 | 0 | 0 | 0 | Pleistocene | CLAYEY MICRITE | Dominat lithology; relative abundance | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 5 | 6 | 0 | 0 |
933.85 | 42-380A-65-21,135 | 0 | 0 | 0 | Pleistocene | MARL | Dominat lithology; relative abundance | 40 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 5 | 0 | 0 | 0 |
933.94 | 42-380A-65-21,144 | 0 | 0 | 0 | Pleistocene | CARBONATE | Minor lithology; relative abundance | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 6 | 0 | 0 | 0 |
934.87 | 42-380A-65-3,87 | 0 | 0 | 0 | Pleistocene | DOLOMITE | Dominat lithology; relative abundance | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 6 | 0 | 0 | 0 |
935.19 | 42-380A-65-31,119 | 0 | 0 | 0 | Pleistocene | CLAY | Dominat lithology; numerical abundance | 10 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 70 | 0 | 0 | 10 | 0 | 0 | 0 |
940.65 | 42-380A-66-1,15 | 0 | 0 | 0 | Pleistocene | CLAYEY ARAGONITE | Minor lithology; numerical abundance | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 0 | 3 | 0 | 0 | 0 |
944.81 | 42-380A-66-31,131 | 0 | 0 | 0 | Pleistocene | CLAY | Minor lithology; relative abundance | 15 | 0 | 0 | 6 | 0 | 6 | 0 | 0 | 0 | 0 | 6 | 60 | 0 | 0 | 15 | 0 | 0 | 0 |
972.75 | 42-380A-69-3,75 | 0 | 0 | 0 | Pleistocene | DOLOMITE | Dominat lithology; relative abundance | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 6 | 0 | 0 | 0 |
981.39 | 42-380A-70-21,139 | 0 | 0 | 0 | Pleistocene | DOLOMITE | Minor lithology; relative abundance | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 6 | 0 | 0 | 0 |
982.32 | 42-380A-70-3,82 | 0 | 0 | 0 | Pleistocene | CLAY | Dominat lithology; relative abundance | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 60 | 0 | 0 | 10 | 6 | 0 | 0 |
982.53 | 42-380A-70-31,103 | 0 | 0 | 0 | Pleistocene | DOLOMITE | Dominat lithology; relative abundance | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 5 | 0 | 0 | 6 | 0 | 0 | 0 |
990.96 | 42-380A-71-21,146 | 0 | 0 | 0 | Pleistocene | DOLOMITE | Minor lithology; numerical abundance | 0 | 93 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
993.39 | 42-380A-71-4,89 | 0 | 25 | 75 | Pleistocene | PYRITE BEARING CLAY | Dominat lithology; numerical abundance | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 75 | 0 | 0 | 10 | 0 | 0 | 0 |
1007.55 | 42-380A-73-1,55 | 0 | 0 | 0 | Pleistocene | DOLOMITE | Dominat lithology; numerical abundance | 30 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
1008.24 | 42-380A-73-11,124.5 | 0 | 20 | 80 | Pleistocene | PYRITE BEARING CLAY | Minor lithology; relative abundance | 3 | 0 | 0 | 6 | 6 | 0 | 0 | 0 | 0 | 0 | 2 | 8 | 0 | 0 | 10 | 0 | 0 | 0 |
1008.25 | 42-380A-73-11,125 | 0 | 40 | 60 | Pleistocene | SILTY CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 6 | 5 | 60 | 6 | 0 | 5 | 0 | 0 | 0 |
1008.26 | 42-380A-73-11,126 | 0 | 25 | 75 | Pleistocene | CLAY | Minor lithology; relative abundance | 5 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 70 | 0 | 0 | 10 | 0 | 0 | 0 |
1008.27 | 42-380A-73-11,127 | 40 | 60 | 0 | Pleistocene | SAND | Minor lithology; relative abundance | 1 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 6 | 3 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
1019.07 | 42-380A-74-21,107 | 0 | 25 | 75 | Pleistocene | CLAY | Dominat lithology; relative abundance | 5 | 0 | 0 | 6 | 6 | 0 | 0 | 0 | 0 | 0 | 5 | 75 | 0 | 0 | 10 | 0 | 0 | 0 |
1019.10 | 42-380A-74-21,110 | 0 | 0 | 0 | Pleistocene | DOLOMITE | Minor lithology; numerical abundance | 0 | 85 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 1 | 0 | 0 | 0 |
1019.45 | 42-380A-74-21,145 | 55 | 45 | 0 | Pleistocene | ZEOLITE RICH QUARTZ SAND | Minor lithology; numerical abundance | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 |
1027.45 | 42-380A-75-11,145 | 0 | 30 | 70 | Pleistocene | CLAY | Dominat lithology; numerical abundance | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 70 | 0 | 0 | 5 | 0 | 0 | 0 |
1027.46 | 42-380A-75-11,146 | 30 | 60 | 10 | Pleistocene | ZEOLITE RICH SILT | Minor lithology; relative abundance | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 5 | 20 | 0 | 0 | 0 | 6 | 0 | 0 |
1036.25 | 42-380A-76-1,75 | 30 | 50 | 20 | Pleistocene | SILTY SAND | Minor lithology; relative abundance | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 5 | 20 | 0 | 0 | 0 | 6 | 0 | 0 |
1066.28 | 42-380A-79-2,78 | 0 | 0 | 0 | Pleistocene | GLASS BEARING CLAY | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 2 | 0 | 8 | 0 | 0 | 3 | 0 | 10 | 0 |
1066.30 | 42-380A-79-2,80 | 5 | 15 | 80 | Pleistocene | CLAY | Dominat lithology; relative abundance | 5 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 80 | 0 | 0 | 0 | 6 | 0 | 0 |
1066.94 | 42-380A-79-21,144 | 0 | 0 | 0 | Pleistocene | DOLOMITE | Dominat lithology; relative abundance | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 6 | 10 | 0 | 0 | 6 | 0 | 0 | 0 |
1074.75 | 42-380A-80-11,125 | 10 | 65 | 25 | SANDY SILT | Dominat lithology; relative abundance | 10 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 10 | 5 | 0 | 0 |