Anonymous (2005): Smear slide analysis of Hole 15-146 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230384
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
Herring, James R; Kaneps, Ansis G; Waterman, Lee S; Schneidermann, Nahum; Riedel, William R; Premoli Silva, Isabella; Prell, Warren L; Nieto, Hernán Perez; Maurrasse, F; Horowitz, Ross M; Hay, William W; Gieskes, Joris M; Donnelly, Thomas W; Broecker, Wallace S; Boyce, Robert E; Bolli, Hans M; Saunders, John B; Edgar, Terence (1973): Initial Reports of the Deep Sea Drilling Project 15. U. S. Government Printing Office, XV, 999 pp, https://doi.org/10.2973/dsdp.proc.15.1973
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 15.116500 * Longitude: -69.377800
Date/Time Start: 1970-12-22T00:00:00 * Date/Time End: 1970-12-22T00:00:00
Minimum DEPTH, sediment/rock: 97.36 m * Maximum DEPTH, sediment/rock: 479.10 m
Event(s):
15-146 * Latitude: 15.116500 * Longitude: -69.377800 * Date/Time: 1970-12-22T00:00:00 * Elevation: -3949.0 m * Penetration: 762 m * Recovery: 145.3 m * Location: Caribbean Sea/BASIN * Campaign: Leg15 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 43 cores; 370 m cored; 4 m drilled; 39.3 % 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 | Chert | Chert | % | Smear slide analysis | fragments | |
14 | Radiolarians | Rad | % | Smear slide analysis | ||
15 | Diatoms | Diatoms | % | Smear slide analysis | ||
16 | Spiculae | Spiculae | % | Smear slide analysis | ||
17 | Minerals, other | Min other | % | Smear slide analysis | ||
18 | Quartz | Qz | % | Smear slide analysis | ||
19 | Feldspar | Fsp | % | Smear slide analysis | ||
20 | Zeolite | Zeo | % | Smear slide analysis | ||
21 | Mica | Mica | % | Smear slide analysis | ||
22 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
23 | Iron | Fe | % | Smear slide analysis | ||
24 | Rutile | Rt | % | Smear slide analysis | ||
25 | Zircon | Zrn | % | Smear slide analysis | ||
26 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
27 | Fecal pellets | Fecal pel | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1719 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 Chert [%] | 14 Rad [%] | 15 Diatoms [%] | 16 Spiculae [%] | 17 Min other [%] | 18 Qz [%] | 19 Fsp [%] | 20 Zeo [%] | 21 Mica [%] | 22 Py [%] | 23 Fe [%] | 24 Rt [%] | 25 Zrn [%] | 26 Volc glass [%] | 27 Fecal pel [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
97.36 | 15-146-1-11,136 | 0 | 0 | 0 | D CLAY | Dominat lithology; relative abundance | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
97.37 | 15-146-1-11,136.5 | 0 | 0 | 85 | CLAY MOTTLED ZONE | Dominat lithology; relative abundance | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
98.60 | 15-146-1-21,110 | 0 | 0 | 85 | CLAY | Dominat lithology; relative abundance | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | |
98.70 | 15-146-1-21,120 | 0 | 0 | 85 | CLAY | Dominat lithology; relative abundance | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | |
99.00 | 15-146-1-3,0 | 0 | 0 | 85 | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
99.60 | 15-146-1-3,60 | 0 | 0 | 85 | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 46 | 0 | |
100.00 | 15-146-1-3,0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | ||||||
100.78 | 15-146-1-4,28 | 0 | 35 | 85 | MOTTLED CLAY | Dominat lithology; relative abundance | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 23 | 23 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 46 | 0 | |
100.83 | 15-146-1-4,33 | 0 | 0 | 85 | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 23 | 0 | 23 | 0 | 0 | 0 | 0 | 46 | 0 | |
102.40 | 15-146-1-5,40 | 0 | 0 | 85 | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | |
102.95 | 15-146-1-5,95 | 0 | 10 | 85 | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | |
103.40 | 15-146-1-51,140 | 0 | 10 | 85 | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | |
103.90 | 15-146-1-6,40 | 0 | 0 | 85 | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | |
104.20 | 15-146-1-6,70 | 0 | 10 | 85 | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | |
104.67 | 15-146-1-61,117 | 0 | 0 | 85 | Upper miocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 |
104.90 | 15-146-1-61,140 | 0 | 10 | 85 | Upper miocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 |
254.61 | 15-146-2-1,32 | 0 | 0 | 1 | Lower miocene | FORAM NANNO CHALK | Dominat lithology; relative abundance | 0 | 0 | 55 | 23 | 0 | 6 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 |
254.71 | 15-146-2-1,42 | 0 | 0 | 1 | Lower miocene | FORAM NANNO CHALK | Dominat lithology; relative abundance | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
257.64 | 15-146-2-3,35 | 0 | 0 | 35 | Lower miocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 75 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
257.99 | 15-146-2-3,70 | 0 | 0 | 0 | Lower miocene | GREEN OOZE | Dominat lithology; relative abundance | 0 | 0 | 75 | 0 | 0 | 23 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
260.94 | 15-146-2-5,65 | 35 | 1 | 35 | Lower miocene | VOLCANIC DEBRIS | Minor lithology; relative abundance | 0 | 0 | 55 | 6 | 0 | 23 | 0 | 6 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 |
261.00 | 15-146-2-5,71 | 10 | 0 | 0 | Lower miocene | VOLCANIC DEBRIS | Minor lithology; relative abundance | 0 | 0 | 55 | 0 | 0 | 23 | 0 | 6 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
261.32 | 15-146-2-51,103 | 1 | 0 | 0 | Lower miocene | VOLCANIC DEBRIS | Minor lithology; relative abundance | 0 | 0 | 55 | 6 | 0 | 0 | 0 | 6 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 |
261.83 | 15-146-2-6,4 | 10 | 0 | 0 | Lower miocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 55 | 6 | 0 | 23 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
261.97 | 15-146-2-6,18 | 0 | 35 | 0 | Lower miocene | RAD NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 55 | 6 | 0 | 23 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 |
262.51 | 15-146-2-6,72 | 10 | 10 | 0 | Lower miocene | RAD NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 55 | 6 | 0 | 23 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 23 | 0 |
263.25 | 15-146-2-61,146 | 10 | 0 | 0 | RAD NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 55 | 6 | 0 | 23 | 6 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | |
422.05 | 15-146-5-1,5 | 1 | 0 | 0 | Lower eocene | ASH | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 75 | 0 | 0 | 0 | 0 | 0 | 23 | 0 |
422.05 | 15-146-5-1,5 | 1 | 0 | 0 | Lower eocene | ASH | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 23 | 0 |
422.05 | 15-146-5-1,5 | 1 | 0 | 0 | Lower eocene | ASH | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 75 | 0 |
422.20 | 15-146-5-1,20 | 0 | 0 | 85 | Lower eocene | CLAY | Minor lithology; relative abundance | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 |
422.55 | 15-146-5-1,55 | 0 | 0 | 0 | Lower eocene | CHALK | Dominat lithology; relative abundance | 0 | 0 | 75 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
423.62 | 15-146-5-2,12 | 0 | 0 | 0 | Upper paleocene | NANNO FORAM CHALK | Dominat lithology; relative abundance | 0 | 1 | 75 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
423.80 | 15-146-5-2,30 | 0 | 0 | 0 | Upper paleocene | CHALK | Dominat lithology; relative abundance | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
424.20 | 15-146-5-2,70 | 0 | 0 | 0 | Upper paleocene | FORAM NANNO CHALK | Dominat lithology; relative abundance | 15 | 0 | 55 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
424.85 | 15-146-5-21,135 | 0 | 0 | 0 | Upper paleocene | CHERT | Minor lithology; relative abundance | 6 | 0 | 75 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
424.90 | 15-146-5-21,140 | 0 | 0 | 0 | Upper paleocene | CHALK? | Dominat lithology; relative abundance | 0 | 0 | 75 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
431.55 | 15-146-6-1,55 | 0 | 0 | 0 | Upper paleocene | CHALK | Dominat lithology; relative abundance | 0 | 0 | 55 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
432.07 | 15-146-6-11,107 | 0 | 0 | 0 | Upper paleocene | CHALK | Dominat lithology; relative abundance | 0 | 0 | 55 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
432.50 | 15-146-6-11,150 | 0 | 0 | 0 | Upper paleocene | CHALK | Dominat lithology; relative abundance | 0 | 0 | 55 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
432.60 | 15-146-6-CC,0 | 0 | 0 | 0 | Upper paleocene | CHALK? | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 23 | 6 | 75 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
432.60 | 15-146-6-CC,0 | 0 | 1 | 0 | Upper paleocene | CHALK? | Dominat lithology; relative abundance | 0 | 0 | 75 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
432.60 | 15-146-6-CC,0 | 0 | 10 | 85 | Upper paleocene | SILICIFIED FRAGMENT | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
440.10 | 15-146-7-1,10 | 0 | 0 | 0 | Upper paleocene | CHALK? | Dominat lithology; relative abundance | 23 | 0 | 55 | 6 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 |
440.15 | 15-146-7-1,15 | 0 | 0 | 85 | Upper paleocene | CHALK? | Dominat lithology; relative abundance | 23 | 0 | 23 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
440.60 | 15-146-7-1,60 | 0 | 10 | 60 | Upper paleocene | CHALK? | Dominat lithology; relative abundance | 23 | 0 | 55 | 23 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
440.67 | 15-146-7-1,67 | 0 | 35 | 35 | Upper paleocene | ASH? | Dominat lithology; relative abundance | 6 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 |
440.80 | 15-146-7-1,80 | 0 | 0 | 85 | Upper paleocene | ASH | Dominat lithology; relative abundance | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 6 | 23 | 0 | 0 | 0 | 0 | 0 | 29 | 0 |
440.84 | 15-146-7-1,84 | 1 | 0 | 35 | Upper paleocene | ASH | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 |
440.94 | 15-146-7-1,94 | 0 | 0 | 35 | Upper paleocene | ASH | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 |
441.16 | 15-146-7-11,116 | 0 | 0 | 0 | CHALK | Dominat lithology; relative abundance | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
441.40 | 15-146-7-11,140 | 0 | 0 | 0 | ASH | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 75 | 0 | |
441.60 | 15-146-7-CC,0 | 0 | 10 | 85 | SILICIFIED FORAMS? | Minor lithology; relative abundance | 0 | 0 | 0 | 6 | 0 | 6 | 0 | 0 | 23 | 0 | 6 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
449.20 | 15-146-8-1,20 | 0 | 10 | 35 | Middle paleocene | SILICIOUS CLAY | Dominat lithology; relative abundance | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 6 | 23 | 0 | 0 | 0 | 0 | 0 | 23 | 0 |
449.60 | 15-146-8-1,60 | 0 | 0 | 85 | Middle paleocene | SILICIOUS CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 |
450.12 | 15-146-8-11,112 | 0 | 10 | 85 | Middle paleocene | SILICIOUS CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 2 | 23 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
451.05 | 15-146-8-2,55 | 0 | 35 | 85 | Middle paleocene | SILICIOUS CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 |
451.32 | 15-146-8-2,82 | 0 | 35 | 85 | Middle paleocene | SILICIOUS CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 23 | 0 | 23 | 0 | 2 | 0 | 0 | 0 | 23 | 0 |
451.41 | 15-146-8-2,91 | 0 | 60 | 0 | Middle paleocene | SILICIOUS CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 29 | 0 |
458.10 | 15-146-9-1,10 | 0 | 35 | 85 | Paleocene | SILICIOUS CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 23 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 |
467.79 | 15-146-10-1,79 | 0 | 1 | 60 | Paleocene | ALTERED VOLCANIC SHARD FRAGMENTS | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 |
468.15 | 15-146-10-11,115 | 0 | 0 | 60 | Paleocene | ALTERED VOLCANIC SHARDS | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 55 | 0 |
468.50 | 15-146-10-11,150 | 0 | 0 | 60 | Paleocene | ALTERED VOLCANIC SHARDS | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 |
469.40 | 15-146-10-2,90 | 0 | 0 | 0 | Paleocene | GLASS SHARDS | Minor lithology; relative abundance | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 75 | 0 |
469.90 | 15-146-10-21,140 | 0 | 0 | 0 | Paleocene | SILICIOUS CLAY | Dominat lithology; relative abundance | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 6 | 0 | 0 | 0 | 1 | 0 | 0 | 6 | 0 |
476.63 | 15-146-11-1,63 | 1 | 0 | 35 | Lower paleocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 2 | 6 | 0 | 0 | 0 | 0 | 55 | 0 |
479.10 | 15-146-11-CC,0 | 0 | 0 | 0 | Upper cretaceous | PELLETS | Minor lithology; relative abundance | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |