Perch-Nielsen, Katharina; Supko, Peter R (2005): Smear slide analysis of Hole 39-355 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230674
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
Perch-Nielsen, Katharina; Supko, Peter R; Boersma, Anne; Bonatti, Enrico; Carlson, Richard L; McCoy, Floyd W; Neprochnov, Yuri P; Zimmerman, H B (1977): Initial Reports of the Deep Sea Drilling Project. U. S. Government Printing Office, XXXIX, 1139 pp, https://doi.org/10.2973/dsdp.proc.39.1977
Further details:
Processed smear slide data base - background and methods. hdl:10013/epic.32353.d001
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: -15.709800 * Longitude: -30.600500
Date/Time Start: 1974-11-08T00:00:00 * Date/Time End: 1974-11-08T00:00:00
Minimum DEPTH, sediment/rock: 55.20 m * Maximum DEPTH, sediment/rock: 443.21 m
Event(s):
39-355 * Latitude: -15.709800 * Longitude: -30.600500 * Date/Time: 1974-11-08T00:00:00 * Elevation: -4901.0 m * Penetration: 461.5 m * Recovery: 117.6 m * Location: South Atlantic/BASIN * Campaign: Leg39 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 22 cores; 209 m cored; 0 m drilled; 56.2 % 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 | Pteropoda | Pteropoda | % | Smear slide analysis | ||
14 | Chert | Chert | % | Smear slide analysis | fragments | |
15 | Radiolarians | Rad | % | Smear slide analysis | ||
16 | Diatoms | Diatoms | % | Smear slide analysis | ||
17 | Spiculae | Spiculae | % | 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 | Clay minerals | Clay min | % | Smear slide analysis | ||
23 | Opaque minerals | Opaque | % | Smear slide analysis | ||
24 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
25 | Iron | Fe | % | Smear slide analysis | ||
26 | Limonite | Lm | % | Smear slide analysis | ||
27 | Heavy minerals | HM | % | Smear slide analysis | ||
28 | Zircon | Zrn | % | Smear slide analysis | ||
29 | Fragments | Fragm | % | Smear slide analysis | calcareous material | |
30 | Micronodules | Micronod | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
2454 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 Pteropoda [%] | 14 Chert [%] | 15 Rad [%] | 16 Diatoms [%] | 17 Spiculae [%] | 18 Qz [%] | 19 Fsp [%] | 20 Zeo [%] | 21 Mica [%] | 22 Clay min [%] | 23 Opaque [%] | 24 Py [%] | 25 Fe [%] | 26 Lm [%] | 27 HM [%] | 28 Zrn [%] | 29 Fragm [%] | 30 Micronod [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
55.20 | 39-355-1-2,50 | 0 | 5 | 95 | Cenozoic | ZEOLITIC MUD | Dominat lithology; relative abundance | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 85 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 5 |
55.25 | 39-355-1-2,55 | 0 | 10 | 90 | Cenozoic | MUD | Dominat lithology; relative abundance | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 2 | 0 | 85 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 1 |
60.55 | 39-355-1-51,135 | 0 | 0 | 0 | Cenozoic | ZEOLITIC MANGANESE MUD | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 2 | 10 | 5 | 5 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
61.95 | 39-355-1-61,125 | 0 | 5 | 95 | Cenozoic | ZEOLITIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 5 | 5 | 2 | 75 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 2 |
62.30 | 39-355-1-CC,0 | 0 | 15 | 85 | Cenozoic | ZEOLITIC MUD | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 5 | 0 | 75 | 0 | 0 | 2 | 0 | 5 | 0 | 0 | 5 |
111.39 | 39-355-2-11,139 | 0 | 40 | 60 | Upper miocene | MUD | Dominat lithology; relative abundance | 0 | 2 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 4 | 0 | 80 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 |
114.11 | 39-355-2-31,111 | 0 | 0 | 0 | Middle miocene | MUD | Dominat lithology; relative abundance | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 4 | 0 | 60 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 2 |
114.38 | 39-355-2-31,138 | 0 | 0 | 0 | Middle miocene | MARLY NANNO OOZE | Dominat lithology; relative abundance | 40 | 2 | 42 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
116.90 | 39-355-2-5,90 | 25 | 25 | 50 | Middle miocene | FORAM NANNO OOZE | Dominat lithology; relative abundance | 30 | 4 | 42 | 10 | 0 | 0 | 0 | 0 | 0 | 10 | 2 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
117.10 | 39-355-2-51,110 | 0 | 0 | 0 | Middle miocene | NANNO OOZE | Dominat lithology; relative abundance | 15 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
117.21 | 39-355-2-51,121 | 0 | 10 | 90 | Middle miocene | ZEOLITIC QUARTZ MUD | Minor lithology; relative abundance | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 10 | 0 | 75 | 2 | 0 | 0 | 5 | 0 | 0 | 0 | 0 |
117.22 | 39-355-2-51,122 | 0 | 0 | 0 | Middle miocene | NANNO OOZE | Dominat lithology; relative abundance | 40 | 0 | 40 | 2 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 |
117.23 | 39-355-2-51,123 | 65 | 0 | 35 | Middle miocene | SANDY FORAM OOZE | Minor lithology; numerical abundance | 30 | 0 | 5 | 40 | 0 | 0 | 0 | 0 | 0 | 20 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
117.24 | 39-355-2-51,124 | 0 | 0 | 0 | Middle miocene | ZEOLITIC MUD | Minor lithology; relative abundance | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 10 | 0 | 75 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 |
117.38 | 39-355-2-51,138 | 0 | 0 | 0 | Middle miocene | NANNO MARL | Minor lithology; relative abundance | 10 | 0 | 40 | 5 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 2 | 0 | 20 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 5 |
117.60 | 39-355-2-CC,0 | 0 | 0 | 0 | Middle miocene | MARLY NANNO OOZE | Dominat lithology; relative abundance | 15 | 2 | 45 | 5 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
167.58 | 39-355-3-1,58 | 0 | 0 | 0 | Lower miocene | ZEOLITIC PELAGIC CLAY | Dominat lithology; numerical abundance | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 70 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 5 |
167.58 | 39-355-3-1,58 | 0 | 0 | 0 | Lower miocene | ZEOLITIC PELAGIC CLAY | Dominat lithology; numerical abundance | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 70 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 5 |
167.63 | 39-355-3-1,63 | 0 | 0 | 0 | Lower miocene | MARLY FORAM NANNO OOZE | Dominat lithology; relative abundance | 30 | 0 | 42 | 8 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 20 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
169.72 | 39-355-3-21,122 | 0 | 0 | 0 | Lower miocene | MARLY FORAM NANNO OOZE | Dominat lithology; relative abundance | 10 | 0 | 50 | 10 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | 5 | 0 | 20 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 |
169.88 | 39-355-3-21,138 | 0 | 0 | 0 | Lower miocene | MARLY FORAM NANNO OOZE | Dominat lithology; numerical abundance | 10 | 0 | 35 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
171.14 | 39-355-3-31,114 | 0 | 0 | 0 | Lower miocene | ZEOLITIC DOLOMITIC PELAGIC CLAY | Dominat lithology; relative abundance | 30 | 10 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 20 | 2 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
171.19 | 39-355-3-31,119 | 0 | 0 | 0 | Lower miocene | ZEOLITIC PELAGIC CLAY | Dominat lithology; numerical abundance | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 |
173.20 | 39-355-3-5,20 | 0 | 0 | 0 | Lower miocene | MARLY ZEOLITIC PELAGIC CLAY | Dominat lithology; numerical abundance | 10 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 50 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 |
174.60 | 39-355-3-CC,0 | 0 | 0 | 0 | Lower miocene | MARLY ZEOLITIC PELAGIC CLAY | Dominat lithology; relative abundance | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 20 | 0 | 50 | 0 | 0 | 0 | 5 | 0 | 2 | 0 | 5 |
215.80 | 39-355-4-11,130 | 0 | 0 | 0 | Middle eocene | PELAGIC CLAY | Dominat lithology; numerical abundance | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 65 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 5 |
218.70 | 39-355-4-31,120 | 0 | 0 | 0 | Middle eocene | ZEOLITIC PELAGIC CLAY | Dominat lithology; relative abundance | 5 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 60 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 |
244.00 | 39-355-5-1,60 | 0 | 0 | 0 | Middle eocene | RAD MUD | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 10 | 0 | 0 | 0 | 0 | 45 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 |
246.77 | 39-355-5-3,37 | 50 | 30 | 20 | Middle eocene | QUARTZOSE SAND | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 40 | 10 | 20 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
248.90 | 39-355-5-41,100 | 0 | 0 | 0 | Middle eocene | ZEOLITIC PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 80 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
251.28 | 39-355-5-6,38 | 50 | 30 | 20 | Middle eocene | ZEOLITIC QUARTZOSE SAND | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 10 | 15 | 0 | 30 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
251.95 | 39-355-5-61,105 | 0 | 50 | 50 | Middle eocene | ZEOLITIC QUARTZOSE SILT | Minor lithology; relative abundance | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 50 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 2 |
263.36 | 39-355-6-1,96 | 0 | 5 | 0 | DOLOMITE ROCK | Dominat lithology; numerical abundance | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
265.63 | 39-355-6-3,23 | 20 | 25 | 45 | SANDY ZEOLITIC DOLOMITIC MUD | Dominat lithology; numerical abundance | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 5 | 25 | 1 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | |
266.45 | 39-355-6-31,105 | 0 | 0 | 0 | ZEOLITE PELAGIC MUD | Dominat lithology; relative abundance | 0 | 5 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 60 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | |
266.98 | 39-355-6-4,8 | 50 | 0 | 50 | ZEOLITE SAND | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 45 | 5 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | |
267.20 | 39-355-6-4,30 | 0 | 25 | 75 | ZEOLITIC MUD | Dominat lithology; numerical abundance | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 55 | 0 | 1 | 5 | 0 | 0 | 0 | 0 | 4 | |
268.71 | 39-355-6-5,31 | 5 | 60 | 35 | QUARTZOSE ZEOLITE PELAGIC CLAY | Dominat lithology; numerical abundance | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 35 | 0 | 50 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | |
269.04 | 39-355-6-5,64 | 5 | 70 | 25 | QUARTZOSE ZEOLITIC PELAGIC CLAY | Dominat lithology; numerical abundance | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 5 | 15 | 0 | 10 | 15 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | |
269.26 | 39-355-6-5,86 | 10 | 30 | 60 | ZEOLITIC PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 35 | 2 | 50 | 0 | 0 | 2 | 10 | 0 | 0 | 0 | 2 | |
271.50 | 39-355-6-CC,0 | 0 | 0 | 0 | DOLOMITE OOZE | Dominat lithology; numerical abundance | 0 | 45 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 40 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | |
282.60 | 39-355-7-2,10 | 70 | 10 | 20 | Eocene | ZEOLITIC QUARTZOSE MUD | Dominat lithology; relative abundance | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 10 | 10 | 5 | 5 | 0 | 5 | 0 | 0 | 5 | 2 | 0 | 0 |
283.00 | 39-355-7-2,50 | 0 | 0 | 0 | Eocene | DOLOMITIC ZEOLITIC PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 50 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
285.00 | 39-355-7-31,100 | 0 | 0 | 0 | Eocene | ZEOLITIC PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 45 | 2 | 40 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 5 |
302.50 | 39-355-8-21,100 | 0 | 0 | 0 | Lower eocene | ZEOLITIC PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 25 | 2 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
319.80 | 39-355-9-1,80 | 0 | 0 | 0 | Lower eocene | ZEOLITIC PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 30 | 0 | 65 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 |
321.80 | 39-355-9-21,130 | 0 | 0 | 0 | Lower eocene | ZEOLITIC PELAGIC CLAY | Dominat lithology; numerical abundance | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
322.08 | 39-355-9-3,8 | 0 | 10 | 90 | Lower eocene | CLAY | Dominat lithology; numerical abundance | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 2 | 1 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
340.34 | 39-355-10-2,84 | 0 | 10 | 90 | Lower eocene | ZEOLITIC PELAGIC CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 88 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
340.60 | 39-355-10-21,110 | 0 | 0 | 0 | Lower eocene | ZEOLITIC PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 30 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
348.48 | 39-355-11-1,98 | 0 | 0 | 0 | Lower eocene | ZEOLITIC PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 20 | 0 | 80 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
349.30 | 39-355-11-2,30 | 0 | 0 | 0 | Lower eocene | ZEOLITIC PELAGIC CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
359.79 | 39-355-12-2,29 | 0 | 0 | 0 | Lower eocene | ZEOLITIC MUD | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 5 | 15 | 3 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
361.70 | 39-355-12-3,70 | 0 | 5 | 95 | Lower eocene | ZEOLITIC PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 5 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
365.23 | 39-355-12-51,123 | 0 | 80 | 20 | Lower eocene | ZEOLITIC QUARTZOSE MUD | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 5 | 10 | 10 | 10 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 |
365.60 | 39-355-12-CC,0 | 5 | 80 | 15 | Lower eocene | QUARTZ MUD | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 85 | 5 | 1 | 1 | 5 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 |
368.21 | 39-355-13-2,21 | 1 | 90 | 10 | Lower eocene | QUARTZ SILT | Dominat lithology; numerical abundance | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 90 | 0 | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 1 |
369.20 | 39-355-13-21,120 | 0 | 70 | 0 | Lower eocene | ZEOLITIC QUARTZ MUD | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 45 | 0 | 20 | 10 | 20 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
377.55 | 39-355-14-2,5 | 5 | 85 | 10 | Lower eocene | QUARTZ MUD | Dominat lithology; numerical abundance | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 5 | 0 | 10 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
378.20 | 39-355-14-2,70 | 0 | 0 | 0 | Lower eocene | ZEOLITIC PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 20 | 0 | 80 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
380.75 | 39-355-14-4,25 | 0 | 5 | 0 | Lower eocene | FERRUGINOUS ZEOLITIC PELAGIC CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 15 | 0 | 70 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 |
382.32 | 39-355-14-5,32 | 0 | 0 | 0 | Lower eocene | ZEOLITIC FERRUGINOUS PELAGIC CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 65 | 5 | 0 | 0 | 20 | 0 | 0 | 0 | 0 |
385.97 | 39-355-15-1,47 | 0 | 80 | 20 | Lower eocene | ZEOLITIC QUARTZ MUD | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 8 | 1 | 10 | 0 | 0 | 1 | 0 | 4 | 0 | 0 | 0 |
386.42 | 39-355-15-1,92 | 0 | 0 | 0 | Lower eocene | CLAYSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 90 | 5 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
387.75 | 39-355-15-2,75 | 0 | 10 | 90 | Lower eocene | FERRUGINOUS CLAYSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 60 | 0 | 0 | 2 | 30 | 0 | 0 | 0 | 5 |
388.02 | 39-355-15-21,102 | 0 | 90 | 10 | Lower eocene | QUARTZ SILT | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 0 | 8 | 5 | 10 | 5 | 0 | 0 | 0 | 10 | 0 | 0 | 0 |
396.40 | 39-355-16-11,140 | 0 | 0 | 100 | FERRUGINOUS CLAYSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 70 | 0 | 0 | 0 | 20 | 0 | 0 | 2 | 0 | |
397.58 | 39-355-16-21,108 | 0 | 0 | 0 | ZEOLITIC PELAGIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 20 | 20 | 2 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
405.80 | 39-355-17-11,130 | 0 | 0 | 0 | Upper senonian | FERRUGINOUS ZEOLITIC CLAYSTONE | Dominat lithology; numerical abundance | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 10 | 5 | 0 | 50 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 |
406.50 | 39-355-17-2,50 | 0 | 25 | 75 | Upper senonian | CALCAREOUS OOZE | Dominat lithology; numerical abundance | 65 | 1 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 0 | 1 |
408.95 | 39-355-17-31,145 | 0 | 0 | 0 | Upper senonian | NANNO CHALK | Dominat lithology; relative abundance | 40 | 2 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
409.20 | 39-355-17-4,20 | 0 | 0 | 0 | Upper senonian | FERRUGINOUS NANNO OOZE | Dominat lithology; relative abundance | 40 | 2 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 |
409.98 | 39-355-17-4,98 | 0 | 0 | 0 | Upper senonian | CARBONATE | Minor lithology; numerical abundance | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
410.87 | 39-355-17-5,37 | 0 | 0 | 0 | Upper senonian | NANNO OOZE | Dominat lithology; relative abundance | 20 | 2 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
411.30 | 39-355-17-5,80 | 0 | 30 | 70 | Upper senonian | NANNO OOZE | Dominat lithology; relative abundance | 45 | 2 | 45 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 2 |
416.15 | 39-355-18-2,65 | 0 | 0 | 0 | Upper senonian | NANNO OOZE | Dominat lithology; relative abundance | 40 | 2 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
417.27 | 39-355-18-3,27 | 0 | 30 | 70 | Upper senonian | NANNO OOZE | Dominat lithology; relative abundance | 25 | 2 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 2 | 0 | 0 | 5 |
425.91 | 39-355-19-2,91 | 0 | 20 | 80 | Upper campanian | NANNO OOZE | Dominat lithology; numerical abundance | 40 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
427.55 | 39-355-19-31,105 | 0 | 20 | 80 | Upper campanian | NANNO OOZE | Dominat lithology; relative abundance | 45 | 2 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 |
435.22 | 39-355-20-2,72 | 0 | 0 | 0 | Campanian | NANNO OOZE | Dominat lithology; relative abundance | 40 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
435.97 | 39-355-20-21,147 | 0 | 0 | 0 | Campanian | NANNO OOZE | Dominat lithology; relative abundance | 30 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
442.62 | 39-355-21-1,12 | 0 | 20 | 80 | Lower campanian | NANNO OOZE | Dominat lithology; relative abundance | 60 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 2 |
442.78 | 39-355-21-1,28 | 0 | 0 | 0 | Lower campanian | NANNO OOZE | Dominat lithology; relative abundance | 45 | 2 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 5 | 2 | 10 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
443.10 | 39-355-21-1,60 | 0 | 0 | 0 | Lower campanian | FERRUGINOUS NANNO OOZE | Dominat lithology; relative abundance | 40 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 10 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 |
443.21 | 39-355-21-1,71 | 0 | 0 | 0 | Lower campanian | LIMESTONE | Minor lithology; numerical abundance | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |