Perch-Nielsen, Katharina; Supko, Peter R (2005): Smear slide analysis of Hole 39-357 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230677
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:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: -30.004200 * Longitude: -35.559800
Date/Time Start: 1974-11-23T00:00:00 * Date/Time End: 1974-11-23T00:00:00
Minimum DEPTH, sediment/rock: 4.40 m * Maximum DEPTH, sediment/rock: 796.25 m
Event(s):
39-357 * Latitude: -30.004200 * Longitude: -35.559800 * Date/Time: 1974-11-23T00:00:00 * Elevation: -2086.0 m * Penetration: 797 m * Recovery: 344.3 m * Location: South Atlantic/CONT RISE * Campaign: Leg39 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 50 cores; 463.5 m cored; 9.5 m drilled; 74.3 % 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 | Lamellibranchiata | Lamellibranchiata | % | 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 | Glauconite | Glt | % | Smear slide analysis | ||
24 | Opaque minerals | Opaque | % | Smear slide analysis | ||
25 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
26 | Limonite | Lm | % | Smear slide analysis | ||
27 | Heavy minerals | HM | % | Smear slide analysis | ||
28 | Apatite | Ap | % | Smear slide analysis | ||
29 | Hornblende | Hbl | % | Smear slide analysis | ||
30 | Amphibole | Amp | % | Smear slide analysis | ||
31 | Pyroxene | Pyrox | % | Smear slide analysis | ||
32 | Volcanic glass | Volc glass | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
2387 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 Lamellibranchiata [%] | 14 Chert [%] | 15 Rad [%] | 16 Diatoms [%] | 17 Spiculae [%] | 18 Qz [%] | 19 Fsp [%] | 20 Zeo [%] | 21 Mica [%] | 22 Clay min [%] | 23 Glt [%] | 24 Opaque [%] | 25 Py [%] | 26 Lm [%] | 27 HM [%] | 28 Ap [%] | 29 Hbl [%] | 30 Amp [%] | 31 Pyrox [%] | 32 Volc glass [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
4.40 | 39-357-1-31,140 | 40 | 20 | 40 | Lower pleistocene | NANNO FORAM OOZE | Dominat lithology; numerical abundance | 0 | 0 | 50 | 44 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
13.30 | 39-357-2-31,140 | 20 | 5 | 75 | Lower pliocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 54 | 36 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 9 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
22.40 | 39-357-3-31,140 | 20 | 5 | 75 | Neogene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 60 | 35 | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 1 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
31.30 | 39-357-4-3,80 | 20 | 5 | 75 | Upper miocene | FORAM NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 65 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
42.28 | 39-357-5-4,78 | 15 | 15 | 70 | Miocene | FORAM NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 65 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 |
53.40 | 39-357-6-5,90 | 10 | 30 | 60 | Miocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 60 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
63.00 | 39-357-7-51,100 | 10 | 40 | 50 | Lower miocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 70 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
71.00 | 39-357-8-41,100 | 10 | 20 | 70 | Lower miocene | FORAM NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 80 | 15 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
79.40 | 39-357-9-31,100 | 5 | 30 | 65 | Lower miocene | FORAM NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 85 | 10 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
96.50 | 39-357-10-21,100 | 5 | 30 | 65 | Lower miocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 75 | 15 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
106.00 | 39-357-11-21,100 | 5 | 20 | 75 | Lower miocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 75 | 10 | 0 | 0 | 5 | 0 | 5 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
114.72 | 39-357-12-2,22 | 0 | 15 | 85 | Lower miocene | FORAM NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 40 | 5 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
117.00 | 39-357-12-31,100 | 5 | 35 | 60 | Lower miocene | FORAM NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 80 | 10 | 0 | 0 | 2 | 0 | 5 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
136.20 | 39-357-13-3,70 | 5 | 30 | 65 | Lower miocene | FORAM NANNO OOZE | Dominat lithology; relative abundance | 2 | 0 | 80 | 10 | 0 | 0 | 2 | 0 | 5 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
137.55 | 39-357-13-4,55 | 5 | 30 | 65 | Lower miocene | FORAM NANNO OOZE | Dominat lithology; relative abundance | 5 | 0 | 75 | 10 | 0 | 0 | 2 | 0 | 5 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
151.07 | 39-357-14-1,7 | 20 | 40 | 40 | Lower miocene | FORAM NANNO OOZE | Dominat lithology; relative abundance | 15 | 0 | 40 | 25 | 0 | 0 | 2 | 0 | 5 | 2 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
153.36 | 39-357-14-2,86 | 10 | 50 | 40 | Lower miocene | FORAM NANNO OOZE | Dominat lithology; relative abundance | 15 | 0 | 35 | 25 | 0 | 0 | 2 | 0 | 5 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 |
172.55 | 39-357-15-21,105 | 0 | 40 | 60 | Tertiary | FORAM NANNO CHALK | Dominat lithology; relative abundance | 15 | 0 | 55 | 15 | 0 | 0 | 2 | 0 | 10 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
181.36 | 39-357-16-2,36 | 0 | 30 | 70 | Upper oligocene | FORAM NANNO CHALK | Dominat lithology; relative abundance | 20 | 0 | 35 | 20 | 0 | 0 | 2 | 0 | 5 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
182.40 | 39-357-16-21,140 | 20 | 50 | 30 | Upper oligocene | FORAM NANNO CHALK | Dominat lithology; relative abundance | 15 | 0 | 45 | 25 | 0 | 0 | 2 | 0 | 5 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
189.90 | 39-357-17-1,90 | 5 | 50 | 45 | Upper oligocene | FORAM NANNO CHALK | Dominat lithology; relative abundance | 10 | 0 | 40 | 30 | 0 | 0 | 2 | 0 | 10 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
210.10 | 39-357-18-2,60 | 5 | 45 | 50 | Upper oligocene | FORAM NANNO CHALK | Dominat lithology; relative abundance | 10 | 0 | 40 | 20 | 0 | 0 | 2 | 0 | 10 | 5 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
211.06 | 39-357-18-3,6 | 0 | 0 | 0 | Upper oligocene | INK CHALK (PYRITE OOZE) | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
238.88 | 39-357-19-2,88 | 10 | 50 | 40 | Lower oligocene | FORAM NANNO CHALK | Dominat lithology; relative abundance | 20 | 0 | 45 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 10 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
256.70 | 39-357-20-11,120 | 0 | 0 | 0 | Upper eocene | FORAM NANNO CHALK | Dominat lithology; numerical abundance | 25 | 0 | 40 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
258.00 | 39-357-20-21,100 | 5 | 45 | 50 | Upper eocene | FORAM NANNO OOZE | Dominat lithology; relative abundance | 10 | 0 | 50 | 30 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
284.75 | 39-357-21-1,75 | 0 | 0 | 0 | Middle eocene | NANNO CHALK | Dominat lithology; numerical abundance | 15 | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
287.30 | 39-357-21-3,30 | 0 | 0 | 0 | Middle eocene | FORAM NANNO CHALK | Dominat lithology; relative abundance | 15 | 0 | 45 | 35 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
287.80 | 39-357-21-3,80 | 20 | 60 | 20 | Middle eocene | FORAM NANNO CHALK | Dominat lithology; relative abundance | 25 | 0 | 40 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
305.33 | 39-357-22-2,83 | 0 | 30 | 70 | Middle eocene | ZEOLITIC CALCAREOUS CHALK | Dominat lithology; relative abundance | 25 | 2 | 30 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 20 | 2 | 5 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
307.00 | 39-357-22-31,100 | 5 | 40 | 55 | Middle eocene | NANNO FORAM CHALK | Dominat lithology; numerical abundance | 20 | 0 | 50 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
307.18 | 39-357-22-31,118 | 0 | 0 | 0 | Middle eocene | CALCAREOUS CHALK | Dominat lithology; relative abundance | 40 | 0 | 35 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 5 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
334.02 | 39-357-23-2,62 | 0 | 30 | 50 | Middle eocene | LIMESTONE | Dominat lithology; numerical abundance | 85 | 0 | 3 | 0 | 0 | 0 | 1 | 1 | 2 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
337.02 | 39-357-23-4,62 | 5 | 30 | 65 | Middle eocene | LIMESTONE-CALCAREOUS CHALK | Dominat lithology; numerical abundance | 80 | 0 | 13 | 3 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
350.89 | 39-357-24-1,39 | 5 | 45 | 50 | Middle eocene | SILICIFIED LIMESTONE | Dominat lithology; relative abundance | 20 | 5 | 30 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 5 | 0 | 5 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 |
354.42 | 39-357-24-3,92 | 0 | 50 | 50 | Middle eocene | SILICIFIED LIMESTONE | Dominat lithology; relative abundance | 20 | 10 | 25 | 2 | 0 | 0 | 2 | 2 | 10 | 0 | 0 | 0 | 0 | 20 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
357.32 | 39-357-24-5,82 | 5 | 50 | 45 | Middle eocene | SILICIFIED LIMESTONE | Dominat lithology; relative abundance | 5 | 5 | 20 | 10 | 0 | 0 | 20 | 2 | 10 | 5 | 5 | 2 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 2 | 5 |
357.37 | 39-357-24-5,87 | 0 | 20 | 80 | Middle eocene | GLAUCONITIC MUDSTONE | Dominat lithology; relative abundance | 5 | 2 | 10 | 0 | 0 | 0 | 5 | 0 | 5 | 2 | 2 | 2 | 0 | 0 | 30 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
357.39 | 39-357-24-5,89 | 0 | 80 | 20 | Middle eocene | DOLOSTONE | Dominat lithology; numerical abundance | 10 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
357.44 | 39-357-24-5,94 | 0 | 80 | 20 | Middle eocene | DOLOSTONE | Dominat lithology; numerical abundance | 10 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
359.00 | 39-357-24-61,100 | 10 | 85 | 5 | Middle eocene | DOLOSTONE | Dominat lithology; numerical abundance | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
359.40 | 39-357-24-61,140 | 0 | 80 | 20 | Middle eocene | DOLOSTONE | Dominat lithology; numerical abundance | 20 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 |
372.92 | 39-357-25-3,41 | 0 | 0 | 0 | Middle eocene | DOLOSTONE | Dominat lithology; relative abundance | 7 | 0 | 2 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 45 |
373.20 | 39-357-25-3,70 | 20 | 60 | 20 | Middle eocene | NOT ACCEPTED FOR DATA | Dominat lithology; relative abundance | 40 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 5 | 20 |
373.23 | 39-357-25-3,73 | 0 | 40 | 60 | Middle eocene | SILICEOUS DOLOMITIC LIMESTONE | Dominat lithology; numerical abundance | 20 | 30 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 |
373.49 | 39-357-25-3,99 | 0 | 0 | 0 | Middle eocene | LIMESTONE | Dominat lithology; relative abundance | 10 | 5 | 40 | 30 | 0 | 5 | 0 | 2 | 0 | 0 | 0 | 5 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
373.60 | 39-357-25-31,110 | 5 | 50 | 45 | Middle eocene | SILICEOUS LIMESTONE | Dominat lithology; relative abundance | 35 | 0 | 30 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
373.75 | 39-357-25-31,125 | 0 | 0 | 0 | Middle eocene | SILICEOUS LIMESTONE (PORCELLANITE ?) | Dominat lithology; relative abundance | 15 | 0 | 20 | 10 | 0 | 0 | 25 | 2 | 10 | 0 | 0 | 5 | 0 | 5 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
386.40 | 39-357-26-51,100 | 0 | 40 | 60 | Middle eocene | FORAM NANNO LIMESTONE | Dominat lithology; relative abundance | 5 | 0 | 50 | 30 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 5 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
413.10 | 39-357-27-4,60 | 5 | 40 | 55 | Middle eocene | SILICEOUS FORAM NANNO LIMESTONE | Dominat lithology; relative abundance | 5 | 2 | 35 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
416.22 | 39-357-27-6,72 | 20 | 40 | 40 | Middle eocene | SILICIFIED LIMESTONE | Dominat lithology; relative abundance | 10 | 0 | 10 | 5 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
438.23 | 39-357-28-2,23 | 0 | 30 | 70 | Middle eocene | SILICEOUS LIMESTONE | Dominat lithology; relative abundance | 20 | 0 | 15 | 10 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 |
441.58 | 39-357-28-4,58 | 10 | 30 | 60 | Middle eocene | SILICIFIED LIMESTONE | Dominat lithology; relative abundance | 30 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
465.30 | 39-357-29-1,80 | 0 | 20 | 80 | Upper paleocene | NANNO LIMESTONE | Dominat lithology; relative abundance | 0 | 0 | 65 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
476.70 | 39-357-30-2,70 | 5 | 25 | 70 | Lower paleocene | LIMESTONE | Dominat lithology; relative abundance | 15 | 2 | 25 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 |
495.90 | 39-357-31-21,140 | 0 | 10 | 90 | Upper maestrichtian | NANNO LIMESTONE | Dominat lithology; numerical abundance | 20 | 5 | 50 | 5 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
496.30 | 39-357-31-3,30 | 10 | 30 | 60 | Upper maestrichtian | MARLY FORAM NANNO LIMESTONE | Dominat lithology; numerical abundance | 0 | 0 | 50 | 20 | 0 | 0 | 0 | 0 | 5 | 5 | 10 | 0 | 0 | 0 | 0 | 5 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 |
509.26 | 39-357-32-5,76 | 5 | 55 | 40 | Upper maestrichtian | FORAM NANNO CHALK | Dominat lithology; relative abundance | 5 | 5 | 45 | 15 | 0 | 0 | 0 | 0 | 5 | 5 | 5 | 0 | 2 | 5 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 |
527.06 | 39-357-33-41,106 | 5 | 25 | 70 | Middle maestrichtian | DOLOMITE NANNO CHALK | Dominat lithology; relative abundance | 0 | 10 | 50 | 10 | 0 | 0 | 0 | 0 | 0 | 5 | 10 | 0 | 0 | 10 | 2 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
555.45 | 39-357-34-4,55 | 5 | 2 | 70 | Lower maestrichtian | FORAM NANNO CHALK | Dominat lithology; relative abundance | 0 | 5 | 50 | 20 | 0 | 0 | 0 | 0 | 0 | 5 | 5 | 10 | 2 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
558.80 | 39-357-34-6,90 | 5 | 25 | 70 | Lower maestrichtian | FORAM NANNO CHALK | Dominat lithology; relative abundance | 10 | 0 | 35 | 20 | 0 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 5 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
582.25 | 39-357-35-3,75 | 5 | 45 | 50 | Lower maestrichtian | NANNO CHALK | Dominat lithology; relative abundance | 5 | 15 | 30 | 10 | 0 | 0 | 0 | 0 | 0 | 5 | 10 | 0 | 5 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
614.60 | 39-357-36-6,10 | 5 | 40 | 55 | Upper senonian | FORAM NANNO CHALK | Dominat lithology; relative abundance | 15 | 5 | 45 | 25 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 5 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 5 |
696.55 | 39-357-40-31,105 | 5 | 35 | 60 | Lower campanian | SILTY CALCAREOUS CHALK | Dominat lithology; relative abundance | 11 | 2 | 25 | 10 | 0 | 0 | 0 | 0 | 0 | 5 | 12 | 2 | 0 | 10 | 0 | 5 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 20 |
697.45 | 39-357-40-4,45 | 0 | 10 | 90 | Lower campanian | VOLCANIC ASH | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 55 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 |
705.30 | 39-357-41-2,80 | 0 | 10 | 90 | Upper santonian | CLAY (ALTERED VOLCANIC ASH) | Dominat lithology; relative abundance | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 10 |
708.50 | 39-357-41-41,100 | 5 | 35 | 60 | Upper santonian | SILTY CALCAREOUS CHALK | Dominat lithology; relative abundance | 10 | 2 | 35 | 10 | 0 | 0 | 0 | 0 | 0 | 5 | 10 | 5 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 |
717.00 | 39-357-42-41,100 | 5 | 35 | 60 | Upper santonian | MARLY LIMESTONE | Dominat lithology; relative abundance | 0 | 2 | 20 | 5 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 10 | 2 | 20 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 15 |
725.93 | 39-357-43-31,150 | 0 | 0 | 0 | Upper santonian | MARLY FORAM NANNO LIMESTONE | Dominat lithology; numerical abundance | 10 | 5 | 30 | 20 | 0 | 0 | 0 | 0 | 0 | 5 | 5 | 5 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 |
738.90 | 39-357-44-6,90 | 0 | 45 | 55 | Upper santonian | MARLY NANNO LIMESTONE | Dominat lithology; numerical abundance | 20 | 5 | 25 | 15 | 0 | 0 | 0 | 0 | 0 | 5 | 5 | 5 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 |
747.00 | 39-357-46-31,100 | 0 | 50 | 50 | Lower santonian | MARLY MUCKY LIMESTONE | Dominat lithology; numerical abundance | 15 | 5 | 30 | 10 | 0 | 0 | 0 | 0 | 0 | 5 | 5 | 5 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 |
753.02 | 39-357-47-3,2 | 0 | 0 | 0 | Lower santonian | MARLY LIMESTONE | Dominat lithology; relative abundance | 25 | 15 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 5 | 2 | 2 | 10 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 |
767.20 | 39-357-48-6,70 | 0 | 30 | 70 | Lower santonian | SILICIFIED LIMESTONE | Dominat lithology; relative abundance | 35 | 10 | 15 | 10 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
776.60 | 39-357-49-6,60 | 0 | 15 | 85 | Lower santonian | SILICIFIED LIMESTONE | Dominat lithology; relative abundance | 30 | 10 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 |
786.90 | 39-357-50-61,100 | 5 | 35 | 60 | Lower santonian | SILICIFIED LIMESTONE | Dominat lithology; numerical abundance | 55 | 1 | 2 | 2 | 0 | 0 | 1 | 0 | 0 | 1 | 0 | 1 | 0 | 3 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
787.20 | 39-357-50-61,130 | 1 | 10 | 90 | Lower santonian | CLAYSTONE (ALTERED VOLCANIC ASH?): M QTZ 1,CLAY.MINS 90,PYR 1-2,ZEOL 1/N | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
796.25 | 39-357-51-61,125 | 0 | 60 | 40 | Lower santonian | CALCAREOUS MUD (ALTERED VOLCANIC ASH?) | Dominat lithology; relative abundance | 5 | 2 | 10 | 5 | 0 | 0 | 0 | 0 | 0 | 10 | 10 | 5 | 0 | 10 | 0 | 5 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 20 |