Andrews, James E; Packham, Gordon (2005): Smear slide analysis of Hole 30-287 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230589
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Andrews, James E; Packham, Gordon; Eade, J V; Holdsworth, B K; Jones, D L; Klein, J; Kroenke, Loren W; Saito, T; Shafik, S; Stoeser, Douglas B; van der Lingen, Gerrit J (1975): Initial Reports of the Deep Sea Drilling Project 30. U. S. Government Printing Office, XXX, 753 pp, https://doi.org/10.2973/dsdp.proc.30.1975
Further details:
Processed smear slide data base - background and methods. hdl:10013/epic.32353.d001
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: -13.911200 * Longitude: 153.265500
Date/Time Start: 1973-05-15T00:00:00 * Date/Time End: 1973-05-15T00:00:00
Minimum DEPTH, sediment/rock: 1.16 m * Maximum DEPTH, sediment/rock: 236.68 m
Event(s):
30-287 * Latitude: -13.911200 * Longitude: 153.265500 * Date/Time: 1973-05-15T00:00:00 * Elevation: -4632.0 m * Penetration: 252 m * Recovery: 68.7 m * Location: South Pacific/Coral Sea * Campaign: Leg30 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 17 cores; 147.5 m cored; 0 m drilled; 46.6 % 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 | Calcareous spicules | Calc spic | % | 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 | Mica | Mica | % | Smear slide analysis | ||
21 | Clay minerals | Clay min | % | Smear slide analysis | ||
22 | Glauconite | Glt | % | Smear slide analysis | ||
23 | Opaque minerals | Opaque | % | Smear slide analysis | ||
24 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
25 | Iron | Fe | % | Smear slide analysis | ||
26 | Magnetite | Fe3O4 | % | Smear slide analysis | ||
27 | Heavy minerals | HM | % | Smear slide analysis | ||
28 | Amphibole | Amp | % | Smear slide analysis | ||
29 | Pyroxene | Pyrox | % | Smear slide analysis | ||
30 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
31 | Basalt | Basalt | % | Smear slide analysis | ||
32 | Micronodules | Micronod | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1949 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 Calc spic [%] | 13 Rad [%] | 14 Diatoms [%] | 15 Silicoflag [%] | 16 Spiculae [%] | 17 Qz [%] | 18 Fsp [%] | 19 Zeo [%] | 20 Mica [%] | 21 Clay min [%] | 22 Glt [%] | 23 Opaque [%] | 24 Py [%] | 25 Fe [%] | 26 Fe3O4 [%] | 27 HM [%] | 28 Amp [%] | 29 Pyrox [%] | 30 Volc glass [%] | 31 Basalt [%] | 32 Micronod [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1.16 | 30-287-1-11,116 | 0 | 0 | 0 | Upper pleistocene | MICRONODULE BEARING GLASS SHARD RICH CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 75 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 4 |
1.45 | 30-287-1-11,145 | 2 | 35 | 63 | Upper pleistocene | FELDSPAR,HEAVY MINERAL,NANNO BEARING VOLCANIC GLASS RICH SILTY CLAY | Dominat lithology; numerical abundance | 0 | 8 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 63 | 0 | 0 | 0 | 0 | 0 | 7 | 4 | 0 | 15 | 0 | 1 |
1.52 | 30-287-1-2,2 | 60 | 30 | 10 | Upper pleistocene | CLAY,NANNO BEARING,HEAVY MINERAL,FELDSPAR RICH VOLCANIC SILTY SAND | Dominat lithology; numerical abundance | 0 | 5 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 25 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 39 | 0 | 0 |
2.08 | 30-287-1-2,58 | 0 | 0 | 0 | Upper pleistocene | OPAQUE AND GLASS SHARD BEARING NANNO OOZE | Dominat lithology; numerical abundance | 10 | 76 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 2 |
2.53 | 30-287-1-21,103 | 0 | 25 | 75 | Upper pleistocene | VOLCANIC GLASS BEARING,NANNO RICH SILTY CLAY | Dominat lithology; numerical abundance | 0 | 15 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 4 | 0 | 2 |
2.80 | 30-287-1-21,130 | 0 | 0 | 0 | Upper pleistocene | GLASS SHARD BEARING MICARB RICH NANNO OOZE | Minor lithology; numerical abundance | 15 | 76 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 1 |
3.30 | 30-287-1-3,30 | 0 | 0 | 0 | Upper pleistocene | GLASS SHARD AND MICARB BEARING NANNO OOZE | Dominat lithology; numerical abundance | 10 | 85 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 |
5.02 | 30-287-1-4,52 | 0 | 5 | 95 | Upper pleistocene | GLASS-BEARING CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 1 |
5.20 | 30-287-1-4,69.5 | 5 | 60 | 35 | Upper pleistocene | FELDSPAR NANNO BEARING GLASS SHARD VOLCANIC CLAYEY SILT | Dominat lithology; numerical abundance | 0 | 5 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 7 | 0 | 0 | 30 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 53 | 0 | 0 |
5.22 | 30-287-1-4,72 | 10 | 90 | 0 | Upper pleistocene | OPAQUE BEARING HEAVY MINERAL RICH FELDSPAR SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 65 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 |
5.89 | 30-287-1-41,139 | 10 | 20 | 70 | Upper pleistocene | OPAQUE FELDSPAR AND NANNO BEARING GLASSSHARD RICH SILTY CLAY | Dominat lithology; numerical abundance | 1 | 10 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 52 | 0 | 4 | 0 | 0 | 0 | 1 | 0 | 0 | 20 | 0 | 2 |
5.99 | 30-287-1-41,149 | 20 | 80 | 3 | Upper pleistocene | MICARB AND HEAVIES BEARING ALTERED VOLCANIC GLASS AND OPAQUE RICH FELDSP | Dominat lithology; numerical abundance | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 60 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 3 | 0 | 0 | 15 | 0 | 0 |
7.62 | 30-287-1-6,12 | 0 | 20 | 80 | Upper pleistocene | GLASS SHARD (ALTERED) BEARING FELDSPAR RICH CLAY | Dominat lithology; numerical abundance | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 12 | 0 | 0 | 78 | 0 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 4 | 0 | 1 |
9.10 | 30-287-1-CC,0 | 0 | 25 | 75 | Upper pleistocene | MICARB FELDSPAR NANNO BEARING GLASS SHARD RICH SILTY CLAY | Dominat lithology; numerical abundance | 3 | 10 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 3 | 0 | 0 | 58 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 20 | 0 | 2 |
19.68 | 30-287-2-2,68 | 0 | 20 | 80 | Upper pleistocene | MICARB VOLCANIC GLASS NANNO AND PLANT DEBRIS BEARING FELDSPAR RICH CLAY | Dominat lithology; numerical abundance | 5 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 1 | 0 | 47 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 |
19.77 | 30-287-2-2,77 | 0 | 0 | 0 | Upper pleistocene | VOLCANIC GLASS AND FORAM BEARING CLAY RICH NANNO OOZE | Dominat lithology; numerical abundance | 10 | 59 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 |
21.85 | 30-287-2-31,135 | 20 | 75 | 5 | Upper pleistocene | FLEDSPAR CLAY MICARB VOLCANIC GLASS BEARING FORAM RICH CARBONATE SILT | Dominat lithology; numerical abundance | 55 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 |
37.30 | 30-287-3-1,80 | 0 | 0 | 0 | Upper pleistocene | FELDSPAR,FORAM ALTERED VOLCANIC GLASS BEARING MICARB AND CLAY RICH NANNO | Dominat lithology; numerical abundance | 55 | 0 | 8 | 0 | 0 | 0 | 0 | 1 | 0 | 5 | 1 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 |
37.68 | 30-287-3-11,118 | 0 | 0 | 0 | Upper pleistocene | MICARB VOLCANIC GLASS BEARING CLAY RICH NANNO OOZE | Dominat lithology; numerical abundance | 5 | 36 | 2 | 0 | 0 | 0 | 0 | 1 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 0 |
38.10 | 30-287-3-CC,0 | 0 | 25 | 75 | Upper pleistocene | FORAM FELDSPAR GLASS SHARD (ALTERED) MICARB BEARING NANNO OOZE | Dominat lithology; numerical abundance | 10 | 67 | 3 | 0 | 0 | 0 | 0 | 1 | 0 | 5 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 2 |
56.72 | 30-287-4-11,122 | 0 | 40 | 60 | Upper pleistocene | FELDSPAR BEARING ALTERED VOLCANIC GLASSSILTY CLAY | Dominat lithology; numerical abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 58 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 3 | 0 | 0 |
58.60 | 30-287-4-CC,0 | 0 | 0 | 0 | Upper pleistocene | FELDSPAR VOLCANIC GLASS CLAY BEARING MICARB RICH NANNO OOZE | Dominat lithology; numerical abundance | 20 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 8 | 0 | 0 |
79.14 | 30-287-5-31,134 | 0 | 20 | 80 | Lower pleistocene | MICARB FELDSPAR VOLCANIC GLASS BEARING SILTY CLAY | Dominat lithology; numerical abundance | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 5 | 1 | 0 | 77 | 1 | 2 | 2 | 0 | 0 | 1 | 0 | 0 | 5 | 0 | 1 |
79.97 | 30-287-5-4,67 | 5 | 75 | 20 | Lower pleistocene | MICARB AND ALTERED GLASS SHARD BEARING NANNO-FORAM SILT | Dominat lithology; numerical abundance | 5 | 30 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 9 | 0 | 0 |
83.20 | 30-287-5-6,90 | 40 | 60 | 0 | Lower pleistocene | DEVITRIFIED GLASS SHARD (PUMICE) ASH | 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 | 100 | 0 | 0 |
83.90 | 30-287-5-CC,0 | 0 | 20 | 80 | Lower pleistocene | NANNO FELDSPAR AND MICARB BEARING VOLCANIC GLASS CLAY | Dominat lithology; numerical abundance | 8 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 65 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 |
94.96 | 30-287-6-11,146 | 0 | 20 | 80 | Upper pliocene | FELDSPAR FORAM NANNO BEARING CLAY | Dominat lithology; numerical abundance | 2 | 5 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 84 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
97.92 | 30-287-6-31,142 | 20 | 60 | 20 | Upper pliocene | NANNO AND VOLCANIC GLASS BEARING CARBONATE FORAM AND CLAY RICH FELDSPAR | Dominat lithology; numerical abundance | 11 | 5 | 20 | 0 | 0 | 0 | 0 | 0 | 15 | 15 | 2 | 0 | 21 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 8 | 0 | 0 |
98.01 | 30-287-6-4,1 | 95 | 0 | 5 | Upper pliocene | NANNO BEARING FORAM SAND | Dominat lithology; numerical abundance | 0 | 5 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
98.82 | 30-287-6-4,82 | 0 | 0 | 0 | Upper pliocene | FORAM AND MICARB BEARING NANNO OOZE | Dominat lithology; numerical abundance | 3 | 93 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
99.60 | 30-287-6-CC,0 | 0 | 20 | 80 | Upper pliocene | NANNO MICARB FELDSPAR AND PLANT DEBRIS BEARING VOLCANIC GLASS (ALTERED) | Dominat lithology; numerical abundance | 5 | 5 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 0 | 51 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 |
114.10 | 30-287-7-CC,0 | 0 | 20 | 80 | Upper pliocene | FELDSPAR AND MICARB BEARING VOLCANIC GLASS AND NANNO RICH CLAY | Dominat lithology; numerical abundance | 8 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 48 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 2 |
131.86 | 30-287-8-1,36 | 20 | 60 | 20 | Upper pliocene | OPAQUE VOLCANIC GLASS BEARING CLAY RICH SANDY CLAYEY SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 2 | 0 | 25 | 1 | 5 | 2 | 0 | 0 | 30 | 0 | 0 | 5 | 0 | 0 |
132.02 | 30-287-8-1,52 | 0 | 20 | 80 | Upper pliocene | MICRONODULES PYRITE FELDSPAR BEARING VOLCANIC GLASS RICH CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | 70 | 0 | 0 | 3 | 0 | 0 | 2 | 0 | 0 | 15 | 0 | 3 |
135.20 | 30-287-8-3,70 | 5 | 45 | 50 | ZEOLITE AND CHLORITE BEARING FELDSPAR AND ALTERED VOLCANIC GLASS RICH SI | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 5 | 10 | 44 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 20 | 0 | 2 | |
136.10 | 30-287-8-CC,0 | 0 | 40 | 60 | HEAVY MINERALS ZEOLITE FELDSPAR BEARING VOLCANIC GLASS RICH SILTY CLAY | Dominat lithology; numerical abundance | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 1 | 0 | 63 | 0 | 0 | 2 | 0 | 0 | 3 | 0 | 0 | 15 | 0 | 1 | |
151.35 | 30-287-9-1,85 | 2 | 18 | 80 | FELDSPAR ZEOLITE AND ALTERED VOLCANIC GLASS BEARING CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 10 | 0 | 73 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | |
155.10 | 30-287-9-CC,0 | 0 | 20 | 80 | VOLCANIC GLASS BEARING FELDSPAR RICH CLAY | Dominat lithology; numerical abundance | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 1 | 0 | 60 | 0 | 2 | 2 | 0 | 0 | 2 | 0 | 0 | 10 | 0 | 1 | |
170.95 | 30-287-10-11,145 | 0 | 30 | 70 | Upper oligocene | FELDSPAR MICARB BEARING GLASS SHARD RICH SILTY CLAY | Dominat lithology; numerical abundance | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | 62 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 1 | 0 |
171.03 | 30-287-10-2,3 | 4 | 36 | 60 | Upper oligocene | FELDSPAR OPAQUE ALTERED GLASS AND ZEOLITE BEARING MICRONODULE RICH SILTY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 10 | 0 | 59 | 0 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 5 | 0 | 20 |
171.50 | 30-287-10-2,50 | 0 | 40 | 60 | Upper oligocene | MICRONODULE BEARING GLASS SHARD SILTY CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 56 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 1 | 35 | 0 | 5 |
172.10 | 30-287-10-21,110 | 0 | 0 | 0 | Upper oligocene | MICARB RICH NANNO OOZE | Dominat lithology; numerical abundance | 15 | 81 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 |
173.43 | 30-287-10-3,93 | 0 | 0 | 0 | Upper oligocene | CALCAREOUS SPICULE AND CLAY BEARING NANNO OOZE | Dominat lithology; numerical abundance | 0 | 87 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
175.60 | 30-287-10-CC,0 | 0 | 0 | 0 | Upper oligocene | MICRONODULE BEARING NANNO OOZE | Dominat lithology; numerical abundance | 0 | 92 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 3 |
179.92 | 30-287-11-1,62 | 0 | 0 | 0 | Middle eocene | OPAQUE? RICH NANNO OOZE | Dominat lithology; numerical abundance | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
180.60 | 30-287-11-11,130 | 0 | 0 | 0 | Middle eocene | CALCEROUS SPICULE AND FORAM BEARING NANNO OOZE | Dominat lithology; numerical abundance | 2 | 88 | 5 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
184.05 | 30-287-11-4,25 | 0 | 85 | 15 | Middle eocene | VOLCANIC GLASS ZEOLITE AND MICARB BEARING NANNO CHALK | Dominat lithology; numerical abundance | 10 | 79 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 |
185.05 | 30-287-11-41,125 | 0 | 0 | 0 | Middle eocene | ZEOLITE AND SPONGE SPICULE BEARING NANNO CHALK | Dominat lithology; relative abundance | 1 | 87 | 2 | 1 | 1 | 0 | 0 | 5 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
188.40 | 30-287-11-CC,0 | 0 | 0 | 0 | Middle eocene | FORAM SPONGE SPICULE BEARING RAD RICH NANNO CHALK | Dominat lithology; numerical abundance | 2 | 77 | 3 | 0 | 20 | 0 | 0 | 5 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
190.53 | 30-287-12-2,53 | 0 | 0 | 0 | Middle eocene | FORAM RAD AND SPONGE SPICULE BEARING NANNO CHALK | Dominat lithology; numerical abundance | 2 | 83 | 3 | 1 | 5 | 0 | 1 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
193.73 | 30-287-12-4,73 | 0 | 100 | 0 | Middle eocene | FORAM AND SPONGE SPICULE BEARING RAD RICH NANNO CHALK | Dominat lithology; numerical abundance | 3 | 75 | 3 | 2 | 11 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
195.80 | 30-287-12-51,130 | 0 | 0 | 0 | Middle eocene | FORAM BEARING MICARB RICH NANNO CHALK | Dominat lithology; relative abundance | 0 | 80 | 5 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
196.10 | 30-287-12-CC,0 | 0 | 0 | 0 | Middle eocene | ZEOLITE AND FORAM BEARING NANNO CHALK | Dominat lithology; numerical abundance | 2 | 85 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
199.20 | 30-287-13-11,120 | 0 | 0 | 0 | Middle eocene | MICARB RICH NANNO CHALK | Dominat lithology; numerical abundance | 15 | 80 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 |
199.43 | 30-287-13-11,143 | 0 | 0 | 0 | Middle eocene | FORAM ZEOLITE AND MICARB BEARING NANNO CHALK | Dominat lithology; numerical abundance | 6 | 85 | 3 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
199.54 | 30-287-13-2,4 | 0 | 0 | 0 | Middle eocene | MICARB NANNO CHALK | Dominat lithology; numerical abundance | 38 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
202.16 | 30-287-13-31,116 | 0 | 0 | 0 | Middle eocene | ZEOLITE AND FORAM BEARING NANNO CHALK | Dominat lithology; numerical abundance | 2 | 87 | 5 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
202.60 | 30-287-13-CC,0 | 0 | 0 | 0 | Middle eocene | MICARB CALCAREOUS SPICULE FORAM BEARING NANNO CHALK | Dominat lithology; numerical abundance | 10 | 58 | 10 | 3 | 0 | 0 | 0 | 1 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
202.60 | 30-287-13-CC,0 | 2 | 83 | 15 | Middle eocene | ZEOLITE FORAM BEARING MICARB RICH NANNO CHALK | Dominat lithology; numerical abundance | 3 | 87 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
212.10 | 30-287-14-CC,0 | 0 | 80 | 20 | Middle eocene | FORAM AND CALCAREOUS SPICULES BEARING MICARB AND ZEOLITE RICH NANNO CHAL | Dominat lithology; relative abundance | 20 | 43 | 4 | 8 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
218.87 | 30-287-15-2,37 | 2 | 70 | 20 | Lower eocene | PYRITE BEARING ZEOLITE AND MICARB RICH NANNO CHALK | Minor lithology; numerical abundance | 20 | 53 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 |
220.10 | 30-287-15-CC,0 | 0 | 90 | 10 | Lower eocene | FORAM AND MICARB BEARING ZEOLITE RICH NANNO CHALK | Dominat lithology; numerical abundance | 10 | 68 | 5 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
236.68 | 30-287-16-1,68.5 | 0 | 40 | 60 | Lower eocene | OPAQUE MINERAL ZEOLITE GLASS SHARD BEARING MICARB NANNO CHALK | Dominat lithology; numerical abundance | 35 | 52 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 7 | 0 | 0 |