Whitmarsh, Robert B; Weser, Oscar E; Ross, David A (2005): Smear slide analysis of Hole 23-219 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230483
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
Supko, Peter R; Manheim, Frank T; Girdler, R W; Coleman, Robert; Stoffers, Peter; Siddiquie, H N; Nigrini, Catherine A; Matter, A; Mallik, Tapas Kumar; Kidd, Robert B; Jipa, Dan Constantin; Fleisher, R L; Boudreaux, J E; Ali, S; Whitmarsh, Robert B; Weser, Oscar E; Ross, David A (1974): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XXIII, 1180 pp, https://doi.org/10.2973/dsdp.proc.23.1974
Further details:
Processed smear slide data base - background and methods. hdl:10013/epic.32353.d001
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 9.029200 * Longitude: 72.877800
Date/Time Start: 1972-03-10T00:00:00 * Date/Time End: 1972-03-10T00:00:00
Minimum DEPTH, sediment/rock: 0.50 m * Maximum DEPTH, sediment/rock: 267.80 m
Event(s):
23-219 * Latitude: 9.029200 * Longitude: 72.877800 * Date/Time: 1972-03-10T00:00:00 * Elevation: -1764.0 m * Penetration: 273 m * Recovery: 172.8 m * Location: Indian Ocean/Arabian Sea/RIDGE * Campaign: Leg23 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 27 cores; 235 m cored; 0 m drilled; 73.5 % 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 | Radiolarians | Rad | % | Smear slide analysis | ||
13 | Diatoms | Diatoms | % | Smear slide analysis | ||
14 | Spiculae | Spiculae | % | Smear slide analysis | ||
15 | Quartz | Qz | % | Smear slide analysis | ||
16 | Feldspar | Fsp | % | Smear slide analysis | ||
17 | Zeolite | Zeo | % | Smear slide analysis | ||
18 | Clay minerals | Clay min | % | Smear slide analysis | ||
19 | Glauconite | Glt | % | Smear slide analysis | ||
20 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
21 | Apatite | Ap | % | Smear slide analysis | ||
22 | Epidote | Ep | % | Smear slide analysis | ||
23 | Volcanic glass | Volc glass | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1671 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 Rad [%] | 13 Diatoms [%] | 14 Spiculae [%] | 15 Qz [%] | 16 Fsp [%] | 17 Zeo [%] | 18 Clay min [%] | 19 Glt [%] | 20 Py [%] | 21 Ap [%] | 22 Ep [%] | 23 Volc glass [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.50 | 23-219-1-1,50 | 0 | 0 | 100 | Upper pleistocene | CLAY-FORAM-VOLCANIC GLASS-RAD BEARING NANNO OOZE | Dominat lithology; numerical abundance | 0 | 71 | 8 | 8 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 8 |
1.40 | 23-219-1-11,140 | 0 | 0 | 100 | Upper pleistocene | FORAM AND VOLCANIC GLASS BEARING DETRITAL RICH NANNO OOZE | Dominat lithology; numerical abundance | 0 | 63 | 5 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 10 |
1.75 | 23-219-1-2,25 | 0 | 0 | 100 | Upper pleistocene | CLAY-RAD-VOLCANIC GLASS BEARING NANNO OOZE | Dominat lithology; numerical abundance | 0 | 65 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 10 |
2.90 | 23-219-1-21,140 | 0 | 0 | 100 | Upper pleistocene | CLAY-FORAM-VOLCANIC GLASS BEARING NANNOOOZE | Dominat lithology; numerical abundance | 0 | 70 | 5 | 5 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 10 |
3.30 | 23-219-1-3,30 | 0 | 0 | 100 | Upper pleistocene | CLAY AND VOLCANIC GLASS BEARING FORAM NANNO OOZE | Dominat lithology; numerical abundance | 0 | 60 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 5 |
3.60 | 23-219-1-3,60 | 0 | 0 | 0 | Upper pleistocene | CLAY AND CARBONATE BEARING FORAM-NANNO OOZE | Dominat lithology; numerical abundance | 10 | 60 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 |
4.40 | 23-219-1-31,140 | 0 | 0 | 0 | Upper pleistocene | CLAY-RAD-VOLCANIC GLASS BEARING FORAM RICH NANNO OOZE | Dominat lithology; numerical abundance | 0 | 65 | 20 | 5 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 5 |
4.90 | 23-219-1-4,40 | 0 | 0 | 100 | Upper pleistocene | CLAY-FORAM-VOLCANIC GLASS BEARING NANNO OOZE | Dominat lithology; numerical abundance | 0 | 85 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 5 |
5.75 | 23-219-1-41,125 | 0 | 0 | 100 | Lower pleistocene | CLAY AND VOLCANIC GLASS BEARING FORAM NANNO OOZE | Dominat lithology; numerical abundance | 0 | 65 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 5 |
6.10 | 23-219-1-CC,0 | 0 | 0 | 100 | Lower pleistocene | CLAY BEARING FORAM RICH NANNO OOZE | Dominat lithology; numerical abundance | 0 | 78 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 2 |
6.70 | 23-219-2-1,70 | 0 | 0 | 5 | Lower pleistocene | CARBONATE-CLAY-DIATOM-SPICULE BEARING FORAM NANNO OOZE | Dominat lithology; numerical abundance | 5 | 60 | 20 | 0 | 5 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
7.30 | 23-219-2-11,130 | 0 | 0 | 0 | Lower pleistocene | SPICULE BEARING FORAM-NANNO OOZE | Dominat lithology; numerical abundance | 0 | 70 | 25 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
8.10 | 23-219-2-2,60 | 0 | 0 | 5 | Lower pleistocene | CLAY AND DIATOM BEARING FORAM RICH NANNO OOZE | Dominat lithology; numerical abundance | 0 | 75 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
8.80 | 23-219-2-21,130 | 0 | 0 | 0 | Lower pleistocene | DIATOM BEARING FORAM RICH NANNO OOZE | Dominat lithology; numerical abundance | 0 | 80 | 15 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
9.90 | 23-219-2-3,90 | 0 | 0 | 100 | Lower pleistocene | CLAY-GLASS-RAD BEARING FORAM RICH NANNO OOZE | Minor lithology; numerical abundance | 0 | 70 | 15 | 5 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 5 |
11.11 | 23-219-2-4,61 | 0 | 0 | 0 | Lower pleistocene | PYRITE BEARING FORAM RICH NANNO OOZE | Minor lithology; numerical abundance | 0 | 60 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 |
12.10 | 23-219-2-5,10 | 0 | 0 | 0 | Lower pleistocene | DIATOM-RAD-VOLCANIC GLASS BEARING FORAM RICH NANNO OOZE | Dominat lithology; numerical abundance | 0 | 65 | 15 | 5 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 |
13.15 | 23-219-2-51,115 | 0 | 0 | 100 | Lower pleistocene | CLAY-DIATOM-VOLCANIC GLASS BEARING FORAM RICH NANNO OOZE | Dominat lithology; numerical abundance | 0 | 65 | 20 | 0 | 5 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 5 |
13.60 | 23-219-2-CC,0 | 0 | 0 | 100 | Lower pleistocene | CLAY BEARING VOLCANIC GLASS AND FORAM RICH NANNO OOZE | Dominat lithology; numerical abundance | 0 | 75 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 10 |
15.80 | 23-219-3-1,80 | 0 | 0 | 0 | Lower pleistocene | CLAY-DIATOM-VOLCANIC GLASS BEARING FORAM RICH NANNO OOZE | Dominat lithology; numerical abundance | 0 | 70 | 15 | 0 | 5 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 5 |
17.00 | 23-219-3-2,50 | 0 | 0 | 100 | Lower pleistocene | FORAM-DIATOM-RAD-CLAY BEARING NANNO OOZE | Dominat lithology; numerical abundance | 0 | 75 | 5 | 5 | 5 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 |
20.10 | 23-219-3-4,60 | 0 | 0 | 0 | Lower pleistocene | CLAY-DIATOM-FORAM-VOLCANIC GLASS BEARING NANNO OOZE | Dominat lithology; numerical abundance | 0 | 78 | 5 | 0 | 10 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 2 |
37.20 | 23-219-5-31,120 | 0 | 0 | 0 | Upper pliocene | FORAM RICH NANNO OOZE | Dominat lithology; numerical abundance | 0 | 85 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
45.80 | 23-219-6-3,80 | 0 | 0 | 0 | Lower pliocene | DIATOM BEARING FORAM RICH NANNO OOZE | Dominat lithology; numerical abundance | 0 | 75 | 20 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
46.30 | 23-219-6-31,130 | 0 | 0 | 0 | Lower pliocene | DIATOM BEARING FORAM RICH NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 15 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
68.55 | 23-219-8-61,105 | 0 | 0 | 0 | Upper miocene | FORAM RICH NANNO OOZE | Dominat lithology; numerical abundance | 0 | 85 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
80.03 | 23-219-10-2,28 | 0 | 0 | 0 | Miocene | NANNO RICH PYRITE | Minor lithology; numerical abundance | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 0 | 0 |
96.70 | 23-219-12-41,120 | 0 | 0 | 0 | Miocene | FORAM RICH NANNO OOZE | Dominat lithology; numerical abundance | 0 | 60 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
119.30 | 23-219-13-1,30 | 0 | 0 | 0 | Miocene | FORAM RICH NANNO OOZE | Dominat lithology; numerical abundance | 0 | 60 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
119.50 | 23-219-13-1,50 | 0 | 0 | 0 | Miocene | FORAM-NANNO CHALK | Dominat lithology; numerical abundance | 0 | 50 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
120.30 | 23-219-13-11,130 | 0 | 0 | 0 | Lower miocene | NANNO RICH FORAM CHALK | Dominat lithology; numerical abundance | 0 | 20 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
125.40 | 23-219-13-5,40 | 0 | 0 | 0 | Lower miocene | NANNO RICH FORAM CHALK | Dominat lithology; numerical abundance | 0 | 30 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
126.20 | 23-219-13-51,120 | 0 | 0 | 0 | Lower miocene | Dominat lithology; numerical abundance | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
129.00 | 23-219-14-11,100 | 0 | 0 | 0 | Lower miocene | NANNO RICH FORAM OOZE | Dominat lithology; numerical abundance | 0 | 20 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 |
130.25 | 23-219-14-2,75 | 0 | 0 | 0 | Lower miocene | NANNO RICH FORAM OOZE | Dominat lithology; numerical abundance | 0 | 15 | 85 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
131.52 | 23-219-14-3,52 | 0 | 0 | 0 | Lower miocene | NANNO-FORAM OOZE | Dominat lithology; numerical abundance | 0 | 35 | 65 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
131.75 | 23-219-14-3,75 | 0 | 0 | 0 | Lower miocene | NANNO RICH FORAM OOZE | Dominat lithology; numerical abundance | 0 | 20 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
133.11 | 23-219-14-4,61 | 0 | 0 | 0 | Lower miocene | NANNO RICH FORAM OOZE | Dominat lithology; numerical abundance | 0 | 20 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
133.40 | 23-219-14-4,90 | 0 | 0 | 0 | Lower miocene | NANNO RICH FORAM OOZE | Dominat lithology; numerical abundance | 0 | 5 | 85 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
134.10 | 23-219-14-5,10 | 0 | 0 | 0 | Lower miocene | NANNO-FORAM OOZE | Dominat lithology; numerical abundance | 0 | 5 | 65 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
135.00 | 23-219-14-51,100 | 0 | 0 | 0 | Lower miocene | ZEOLITE BEARING NANNO RICH FORAM OOZE | Dominat lithology; numerical abundance | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
136.85 | 23-219-14-61,135 | 0 | 0 | 0 | Lower miocene | NANNO RICH FORAM OOZE | Dominat lithology; numerical abundance | 0 | 20 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
157.23 | 23-219-15-1,75 | 0 | 0 | 0 | Middle oligocene | ZEOLITE BEARING FORAM RICH NANNO OOZE | Dominat lithology; numerical abundance | 0 | 70 | 20 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 |
158.18 | 23-219-15-2,20 | 0 | 0 | 0 | Middle oligocene | ZEOLITE BEARING FORAM RICH NANNO CHALK | Dominat lithology; numerical abundance | 0 | 70 | 20 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 |
160.18 | 23-219-15-3,70 | 0 | 0 | 0 | Middle oligocene | FORAM RICH NANNO CHALK | Dominat lithology; numerical abundance | 0 | 75 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
160.28 | 23-219-15-3,80 | 0 | 0 | 0 | Middle oligocene | ZEOLITE BEARING FORAM RICH NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 78 | 20 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
161.68 | 23-219-15-4,70 | 0 | 0 | 0 | Middle oligocene | ZEOLITE BEARING FORAM RICH NANNO CHALK | Dominat lithology; numerical abundance | 0 | 83 | 15 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
163.08 | 23-219-15-5,60 | 0 | 0 | 0 | Middle oligocene | FORAM RICH NANNO CHALK | Dominat lithology; relative abundance | 0 | 80 | 20 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
184.05 | 23-219-18-1,75 | 0 | 0 | 0 | Upper eocene | SPICULE AND FORAM BEARING NANNO OOZE | Dominat lithology; numerical abundance | 0 | 80 | 10 | 0 | 2 | 8 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
185.55 | 23-219-18-2,75 | 0 | 0 | 0 | Upper eocene | FORAM AND SPICULE BEARING NANNO OOZE | Dominat lithology; numerical abundance | 0 | 80 | 10 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
187.07 | 23-219-18-3,77 | 0 | 0 | 0 | Middle eocene | GLAUCONITE-FORAM-SPICULE BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 85 | 5 | 0 | 0 | 5 | 0 | 2 | 0 | 0 | 5 | 0 | 0 | 0 | 0 |
188.53 | 23-219-18-4,73 | 0 | 0 | 0 | Middle eocene | SPICULE RICH NANNO OOZE | Dominat lithology; relative abundance | 0 | 90 | 0 | 0 | 2 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
190.05 | 23-219-18-5,75 | 0 | 0 | 0 | Middle eocene | FORAM AND SPICULE BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 85 | 5 | 0 | 2 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
191.55 | 23-219-18-6,75 | 0 | 0 | 0 | Middle eocene | FORAM AND SPICULE BEARING RAD RICH NANNO CHALK | Dominat lithology; relative abundance | 0 | 80 | 5 | 10 | 2 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
193.15 | 23-219-19-1,75 | 0 | 0 | 0 | Middle eocene | FORAM-RAD-DIAT-SPICULE BEARING NANNO OOZE | Dominat lithology; numerical abundance | 0 | 80 | 5 | 5 | 5 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
194.65 | 23-219-19-2,75 | 0 | 0 | 0 | Middle eocene | FORAM DIAT RAD BEARING SPICULE RICH NANNO OOZE | Dominat lithology; numerical abundance | 0 | 75 | 5 | 5 | 5 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
196.15 | 23-219-19-3,75 | 0 | 0 | 0 | Middle eocene | DIATOM AND SPICULE BEARING NANNO CHALK | Dominat lithology; relative abundance | 0 | 85 | 2 | 2 | 5 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
197.65 | 23-219-19-4,75 | 0 | 0 | 0 | Middle eocene | DIAT FORAM RAD SPICULE BEARING NANNO OOZE | Dominat lithology; numerical abundance | 0 | 80 | 5 | 5 | 5 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
199.15 | 23-219-19-5,75 | 0 | 0 | 0 | Middle eocene | DIATOM AND FORAM BEARING SPICULE AND RAD RICH NANNO OOZE | Dominat lithology; numerical abundance | 0 | 70 | 5 | 10 | 5 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
200.70 | 23-219-19-6,80 | 0 | 0 | 0 | Middle eocene | SPICULE BEARING FORAM RICH NANNO OOZE | Dominat lithology; numerical abundance | 0 | 80 | 15 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
202.25 | 23-219-20-11,125 | 0 | 0 | 0 | Middle eocene | FORAM AND SPONGE SPICULE BEARING RAD RICH NANNO OOZE | Dominat lithology; numerical abundance | 0 | 60 | 10 | 20 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
203.71 | 23-219-20-21,121 | 0 | 0 | 0 | Middle eocene | FORAM AND SPONGE SPICULE BEARING RAD RICH NANNO OOZE | Dominat lithology; numerical abundance | 0 | 60 | 10 | 20 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
204.82 | 23-219-20-3,82 | 0 | 0 | 0 | Middle eocene | FORAM SPICULE RAD RICH NANNO OOZE | Dominat lithology; numerical abundance | 0 | 55 | 5 | 5 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
206.30 | 23-219-20-4,80 | 0 | 0 | 0 | Middle eocene | SPICULE BEARING RAD RICH NANNO CHALK | Dominat lithology; numerical abundance | 0 | 60 | 0 | 30 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
207.90 | 23-219-20-5,90 | 0 | 0 | 0 | Middle eocene | SPICULE AND RAD RICH NANNO CHALK | Dominat lithology; numerical abundance | 0 | 65 | 0 | 20 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
212.80 | 23-219-21-21,130 | 0 | 0 | 0 | Middle eocene | SPICULE AND RAD RICH NANNO OOZE/CHALK | Dominat lithology; numerical abundance | 0 | 50 | 0 | 30 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
214.40 | 23-219-21-31,140 | 0 | 0 | 0 | Middle eocene | SPICULE AND RAD RICH NANNO CHALK | Dominat lithology; relative abundance | 0 | 50 | 2 | 30 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
215.50 | 23-219-21-41,100 | 0 | 0 | 0 | Middle eocene | SPICULE AND RAD RICH NANNO OOZE | Dominat lithology; numerical abundance | 0 | 60 | 0 | 5 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
247.40 | 23-219-25-11,140 | 0 | 0 | 0 | Lower eocene | NANNO RICH FORAM CHALK | Dominat lithology; numerical abundance | 0 | 15 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 |
247.45 | 23-219-25-11,145 | 0 | 0 | 0 | Lower eocene | FELSPAR FORAM BEARING RAD RICH DETRITAL CLAY | Minor lithology; relative abundance | 0 | 0 | 10 | 20 | 2 | 0 | 0 | 10 | 0 | 60 | 0 | 0 | 2 | 0 | 0 |
247.60 | 23-219-25-CC,0 | 0 | 0 | 0 | Lower eocene | DETRITAL SAND RICH FORAM CHALK | Dominat lithology; numerical abundance | 0 | 0 | 80 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
256.60 | 23-219-26-CC,0 | 0 | 0 | 100 | Lower eocene | NANNO BEARING FORAM DETRITAL CLAY WITH CHERT FRAGMENTS | Dominat lithology; numerical abundance | 50 | 5 | 26 | 0 | 0 | 0 | 0 | 0 | 0 | 19 | 0 | 0 | 0 | 0 | 0 |
264.70 | 23-219-27-1,70 | 50 | 30 | 20 | Upper paleocene | CARBONATE CLAY SILTY SAND | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
265.30 | 23-219-27-11,130 | 0 | 0 | 0 | Upper paleocene | CHALK | Dominat lithology; relative abundance | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 |
265.40 | 23-219-27-11,140 | 0 | 0 | 0 | Upper paleocene | DETRITAL CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | 0 | 2 | 0 |
267.80 | 23-219-27-3,80 | 40 | 30 | 30 | Upper paleocene | CLAYEY SILTY SAND CHALK | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |