Perch-Nielsen, Katharina; Supko, Peter R (2005): Smear slide analysis of Hole 39-356. PANGAEA, https://doi.org/10.1594/PANGAEA.230675
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: -28.287000 * Longitude: -41.088000
Date/Time Start: 1974-11-16T00:00:00 * Date/Time End: 1974-11-16T00:00:00
Minimum DEPTH, sediment/rock: 10.41 m * Maximum DEPTH, sediment/rock: 737.04 m
Event(s):
39-356 * Latitude: -28.287000 * Longitude: -41.088000 * Date/Time: 1974-11-16T00:00:00 * Elevation: -3175.0 m * Penetration: 741 m * Recovery: 310.6 m * Location: South Atlantic/PLATEAU * Campaign: Leg39 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 42 cores; 396 m cored; 9.5 m drilled; 78.4 % 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 | Siliceous microfossils | Silic foss | % | Smear slide analysis | other siliceous material | |
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 | Iron | Fe | % | Smear slide analysis | ||
27 | Limonite | Lm | % | Smear slide analysis | ||
28 | Heavy minerals | HM | % | Smear slide analysis | ||
29 | Zircon | Zrn | % | Smear slide analysis | ||
30 | Topaz | Tpz | % | Smear slide analysis | ||
31 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
32 | Manganese | Mn | % | Smear slide analysis | ||
33 | Micronodules | Micronod | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
3392 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 Silic foss [%] | 15 Rad [%] | 16 Diatoms [%] | 17 Spiculae [%] | 18 Qz [%] | 19 Fsp [%] | 20 Zeo [%] | 21 Mica [%] | 22 Clay min [%] | 23 Glt [%] | 24 Opaque [%] | 25 Py [%] | 26 Fe [%] | 27 Lm [%] | 28 HM [%] | 29 Zrn [%] | 30 Tpz [%] | 31 Volc glass [%] | 32 Mn [%] | 33 Micronod [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
10.41 | 39-356-2-1,51 | 0 | 0 | 0 | Eocene | FORAM NANNO OOZE | Dominat lithology; relative abundance | 5 | 0 | 60 | 15 | 0 | 0 | 0 | 0 | 5 | 4 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
10.75 | 39-356-2-1,85 | 0 | 0 | 0 | Pliocene | ZEOL FORAM NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 61 | 20 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
10.79 | 39-356-2-1,89 | 0 | 0 | 0 | Pliocene | FORAM NANNO OOZE | Dominat lithology; relative abundance | 10 | 0 | 41 | 30 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
39.78 | 39-356-3-11,128 | 0 | 0 | 0 | Lower miocene | NANNO FORAM OOZE | Dominat lithology; relative abundance | 5 | 0 | 25 | 40 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 5 | 2 | 10 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
42.17 | 39-356-3-3,67 | 0 | 0 | 0 | Lower miocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 20 | 0 | 35 | 15 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
44.73 | 39-356-3-5,23 | 0 | 0 | 0 | Lower miocene | TERRIGENOUS CALC OOZE | Dominat lithology; relative abundance | 20 | 0 | 30 | 10 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
47.41 | 39-356-3-61,141 | 0 | 0 | 0 | Lower miocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 15 | 0 | 25 | 20 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 10 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
59.50 | 39-356-4-2,70 | 0 | 0 | 0 | Lower miocene | FORAM NANNO OOZE | Dominat lithology; relative abundance | 15 | 0 | 40 | 20 | 0 | 0 | 2 | 2 | 5 | 10 | 0 | 5 | 0 | 0 | 0 | 4 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
63.89 | 39-356-4-5,59 | 90 | 0 | 10 | Lower miocene | VOLC ASH | Dominat lithology; relative abundance | 5 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 90 | 0 | 0 |
85.96 | 39-356-5-1,6 | 0 | 0 | 0 | Lower miocene | SILICEOUS CALC OOZE | Dominat lithology; relative abundance | 10 | 2 | 25 | 20 | 0 | 0 | 15 | 5 | 5 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 5 | 0 | 0 |
86.90 | 39-356-5-11,100 | 0 | 0 | 0 | Lower miocene | MARLY CALC OOZE | Dominat lithology; relative abundance | 10 | 0 | 15 | 15 | 0 | 0 | 5 | 0 | 5 | 20 | 0 | 5 | 0 | 10 | 0 | 4 | 0 | 0 | 2 | 0 | 0 | 0 | 5 | 0 | 0 |
94.15 | 39-356-5-6,75 | 0 | 0 | 0 | Lower miocene | SILTY NANNO MUD | Dominat lithology; relative abundance | 10 | 0 | 35 | 15 | 0 | 0 | 10 | 0 | 5 | 10 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 5 | 0 | 0 |
114.80 | 39-356-6-1,80 | 0 | 0 | 0 | Lower miocene | MARLY NANNO OOZE | Dominat lithology; relative abundance | 10 | 0 | 30 | 10 | 0 | 0 | 15 | 10 | 8 | 15 | 0 | 0 | 0 | 10 | 0 | 5 | 0 | 0 | 2 | 0 | 0 | 0 | 4 | 0 | 0 |
116.84 | 39-356-6-21,134 | 0 | 0 | 0 | Middle eocene | CALC SILICEOUS OOZE | Dominat lithology; numerical abundance | 10 | 0 | 20 | 10 | 0 | 0 | 15 | 15 | 10 | 10 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
119.50 | 39-356-6-41,100 | 0 | 0 | 0 | Middle eocene | CALC SILICEOUS OOZE | Dominat lithology; relative abundance | 10 | 0 | 20 | 10 | 0 | 0 | 20 | 15 | 10 | 5 | 0 | 2 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
134.00 | 39-356-7-1,50 | 0 | 0 | 0 | Middle eocene | SILICEOUS CALC OOZE | Dominat lithology; relative abundance | 10 | 0 | 15 | 20 | 0 | 0 | 15 | 15 | 5 | 5 | 2 | 4 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
138.60 | 39-356-7-4,60 | 0 | 0 | 0 | Middle eocene | SILICEOUS NANNO OOZE | Dominat lithology; relative abundance | 5 | 0 | 25 | 5 | 0 | 0 | 15 | 10 | 10 | 10 | 2 | 5 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 |
164.05 | 39-356-8-21,105 | 0 | 0 | 0 | Middle eocene | NANNO SILICEOUS OOZE | Dominat lithology; numerical abundance | 5 | 0 | 20 | 0 | 0 | 0 | 25 | 15 | 10 | 5 | 0 | 5 | 0 | 10 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
191.99 | 39-356-9-2,49 | 0 | 0 | 0 | Middle eocene | SILICEOUS NANNO OOZE | Dominat lithology; relative abundance | 10 | 0 | 45 | 5 | 0 | 0 | 10 | 10 | 10 | 5 | 0 | 2 | 0 | 5 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
192.93 | 39-356-9-21,143 | 0 | 0 | 0 | Middle eocene | SILICEOUS CALC OOZE | Dominat lithology; relative abundance | 5 | 4 | 25 | 15 | 0 | 0 | 15 | 10 | 10 | 5 | 0 | 5 | 0 | 5 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
222.35 | 39-356-10-3,85 | 0 | 0 | 0 | Lower eocene | NANNO CHALK | Dominat lithology; relative abundance | 10 | 0 | 40 | 10 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 10 | 0 | 15 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
223.73 | 39-356-10-4,73 | 0 | 0 | 0 | Lower eocene | SILICEOUS LIMESTONE | Dominat lithology; relative abundance | 15 | 0 | 2 | 25 | 0 | 20 | 0 | 10 | 0 | 10 | 0 | 10 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
223.73 | 39-356-10-4,73 | 0 | 0 | 0 | Lower eocene | SILICEOUS LIMESTONE | Dominat lithology; relative abundance | 15 | 0 | 2 | 25 | 0 | 20 | 0 | 10 | 0 | 10 | 0 | 10 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
223.86 | 39-356-10-4,86 | 0 | 0 | 0 | Lower eocene | ZEOL NANNO CHALK | Dominat lithology; numerical abundance | 10 | 0 | 30 | 20 | 0 | 0 | 0 | 5 | 0 | 8 | 0 | 15 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
237.95 | 39-356-11-1,45 | 0 | 0 | 0 | Lower eocene | SILICIFIED LIMESTONE | Dominat lithology; relative abundance | 10 | 0 | 20 | 0 | 0 | 25 | 15 | 0 | 0 | 5 | 0 | 10 | 0 | 15 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
239.32 | 39-356-11-2,32 | 0 | 0 | 0 | Lower eocene | SILICEOUS LIMESTONE | Dominat lithology; relative abundance | 10 | 0 | 15 | 10 | 0 | 20 | 0 | 4 | 0 | 0 | 0 | 20 | 0 | 20 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 5 |
239.70 | 39-356-11-2,70 | 0 | 0 | 0 | Lower eocene | DOLOMITIC FORAM LIMESTONE | Dominat lithology; relative abundance | 10 | 20 | 10 | 25 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
247.97 | 39-356-12-1,97 | 0 | 0 | 0 | Lower eocene | SILICEOUS LIMESTONE | Dominat lithology; numerical abundance | 10 | 0 | 10 | 20 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
249.00 | 39-356-12-2,50 | 0 | 0 | 0 | Lower eocene | ZEOL NANNO CHALK | Dominat lithology; numerical abundance | 10 | 0 | 40 | 15 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 20 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
258.25 | 39-356-13-2,25 | 0 | 0 | 0 | Lower eocene | SILICEOUS NANNO CHALK | Dominat lithology; relative abundance | 5 | 0 | 30 | 5 | 0 | 20 | 0 | 0 | 0 | 5 | 0 | 13 | 5 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
258.65 | 39-356-13-2,65 | 0 | 0 | 0 | Lower eocene | FORAM CHALK | Dominat lithology; relative abundance | 10 | 2 | 5 | 70 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
266.60 | 39-356-14-1,60 | 0 | 0 | 0 | Lower eocene | SILICEOUS NANNO CHALK | Dominat lithology; numerical abundance | 15 | 0 | 20 | 10 | 0 | 25 | 0 | 0 | 0 | 5 | 0 | 10 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
276.69 | 39-356-15-11,119 | 50 | 50 | 0 | Lower eocene | SILICEOUS FORAM CHALK | Dominat lithology; numerical abundance | 30 | 0 | 0 | 35 | 0 | 20 | 0 | 10 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
279.50 | 39-356-15-31,100 | 0 | 0 | 0 | Lower eocene | MARLY NANNO CHALK | Dominat lithology; relative abundance | 10 | 0 | 30 | 15 | 0 | 10 | 0 | 0 | 0 | 5 | 0 | 10 | 0 | 20 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
286.70 | 39-356-16-2,20 | 0 | 0 | 0 | Lower eocene | SILICEOUS NANNO CHALK | Dominat lithology; relative abundance | 10 | 2 | 30 | 10 | 0 | 20 | 0 | 0 | 0 | 8 | 0 | 5 | 0 | 10 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
287.97 | 39-356-16-21,147 | 0 | 0 | 0 | Upper paleocene | MARLY NANNO CHALK | Dominat lithology; relative abundance | 10 | 2 | 35 | 2 | 0 | 0 | 0 | 0 | 0 | 20 | 4 | 5 | 5 | 15 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
295.70 | 39-356-17-1,80 | 0 | 0 | 0 | Upper paleocene | MARLY NANNO CHALK | Dominat lithology; numerical abundance | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 5 | 10 | 10 | 20 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
298.04 | 39-356-17-3,14 | 0 | 0 | 0 | Upper paleocene | MARLY ZEOL NANNO CHALK OOZE | Dominat lithology; relative abundance | 10 | 0 | 40 | 8 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 15 | 4 | 10 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
354.50 | 39-356-23-21,100 | 0 | 0 | 0 | Upper paleocene | ZEOL NANNO CHALK | Dominat lithology; relative abundance | 10 | 0 | 40 | 10 | 0 | 0 | 0 | 2 | 0 | 5 | 0 | 15 | 5 | 15 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
355.71 | 39-356-23-3,71 | 0 | 0 | 0 | Upper paleocene | ZEOL FORAM NANNO CHALK | Dominat lithology; relative abundance | 5 | 0 | 30 | 20 | 0 | 0 | 2 | 2 | 0 | 5 | 5 | 18 | 0 | 10 | 0 | 4 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
363.55 | 39-356-24-2,70 | 0 | 0 | 0 | Middle paleocene | FORAMS NANNO CHALK | Dominat lithology; numerical abundance | 10 | 0 | 45 | 15 | 0 | 0 | 0 | 5 | 0 | 5 | 0 | 10 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
366.14 | 39-356-24-4,29 | 0 | 0 | 0 | Middle paleocene | MARLY SILICEOUS CHALK | Dominat lithology; relative abundance | 10 | 0 | 10 | 25 | 0 | 0 | 15 | 5 | 0 | 10 | 0 | 10 | 2 | 10 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
366.20 | 39-356-24-4,35 | 0 | 0 | 0 | Middle paleocene | MARLY CALC CHALK | Dominat lithology; relative abundance | 5 | 2 | 20 | 25 | 0 | 0 | 5 | 5 | 0 | 20 | 5 | 13 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
366.22 | 39-356-24-4,37 | 0 | 0 | 0 | Middle paleocene | NANNO CHALK | Dominat lithology; relative abundance | 10 | 0 | 60 | 10 | 0 | 0 | 2 | 0 | 5 | 4 | 0 | 5 | 0 | 5 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
366.24 | 39-356-24-4,39 | 0 | 0 | 0 | Middle paleocene | NANNO CHALK | Dominat lithology; relative abundance | 10 | 0 | 60 | 10 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 2 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
372.95 | 39-356-25-2,95 | 0 | 0 | 0 | Lower paleocene | MARLY NANNO CHALK | Dominat lithology; numerical abundance | 10 | 0 | 40 | 10 | 0 | 0 | 10 | 0 | 0 | 8 | 0 | 10 | 0 | 10 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
374.50 | 39-356-25-31,100 | 0 | 0 | 0 | Lower paleocene | NANNO CHALK | Dominat lithology; relative abundance | 10 | 0 | 60 | 10 | 0 | 0 | 10 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
382.85 | 39-356-26-21,100 | 0 | 0 | 0 | Lower paleocene | FORAM NANNO CHALK | Dominat lithology; relative abundance | 10 | 0 | 40 | 20 | 0 | 0 | 10 | 0 | 0 | 5 | 0 | 4 | 0 | 10 | 0 | 4 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 |
386.65 | 39-356-26-5,30 | 0 | 0 | 0 | Lower paleocene | NANNO CHALK | Dominat lithology; relative abundance | 10 | 0 | 45 | 10 | 0 | 0 | 10 | 0 | 0 | 5 | 2 | 10 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
393.50 | 39-356-27-3,75 | 0 | 0 | 0 | Lower paleocene | FORAM NANNO CHALK | Dominat lithology; relative abundance | 5 | 0 | 40 | 20 | 0 | 0 | 10 | 0 | 0 | 5 | 0 | 5 | 0 | 10 | 0 | 4 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 |
397.95 | 39-356-27-6,70 | 0 | 0 | 0 | Lower paleocene | FORAM NANNO CHALK | Dominat lithology; numerical abundance | 10 | 0 | 40 | 20 | 0 | 0 | 10 | 0 | 0 | 5 | 0 | 5 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
402.75 | 39-356-28-3,75 | 0 | 0 | 0 | Lower paleocene | FORAM NANNO CHALK | Dominat lithology; relative abundance | 10 | 0 | 30 | 20 | 0 | 0 | 10 | 0 | 0 | 5 | 4 | 4 | 2 | 10 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
404.70 | 39-356-28-41,120 | 0 | 0 | 0 | Lower paleocene | TERRIGENOUS CALC MUD | Dominat lithology; relative abundance | 0 | 2 | 15 | 10 | 0 | 0 | 8 | 0 | 0 | 20 | 10 | 5 | 2 | 15 | 0 | 5 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 |
407.50 | 39-356-28-61,100 | 0 | 0 | 0 | Lower paleocene | DOLOMITIC CALC CHALK | Dominat lithology; relative abundance | 25 | 10 | 30 | 10 | 0 | 0 | 10 | 0 | 0 | 5 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
408.85 | 39-356-29-1,35 | 0 | 0 | 0 | Lower paleocene | CALC MUD | Dominat lithology; numerical abundance | 5 | 0 | 15 | 8 | 0 | 0 | 5 | 0 | 0 | 20 | 10 | 0 | 0 | 30 | 0 | 5 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
411.70 | 39-356-29-3,20 | 0 | 0 | 0 | Lower paleocene | MARLY CALC CHALK | Dominat lithology; relative abundance | 15 | 0 | 15 | 20 | 0 | 0 | 15 | 0 | 0 | 10 | 5 | 0 | 2 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
412.25 | 39-356-29-3,75 | 0 | 0 | 0 | Upper maestrichtian | NANNO CHALK | Dominat lithology; relative abundance | 20 | 5 | 50 | 5 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 2 | 10 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
415.25 | 39-356-29-5,75 | 0 | 0 | 0 | Upper maestrichtian | NANNO CHALK | Dominat lithology; numerical abundance | 10 | 0 | 55 | 10 | 0 | 0 | 10 | 0 | 0 | 5 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
422.10 | 39-356-30-31,100 | 0 | 0 | 0 | Upper maestrichtian | FORAMS NANNO CHALK | Dominat lithology; relative abundance | 15 | 0 | 45 | 25 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 2 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
426.05 | 39-356-30-6,45 | 0 | 0 | 0 | Upper maestrichtian | FORAM NANNO CHALK | Dominat lithology; relative abundance | 0 | 0 | 65 | 15 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 0 | 0 | 10 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
439.65 | 39-356-31-2,75 | 0 | 0 | 0 | Upper maestrichtian | MARLY NANNO CHALK | Dominat lithology; numerical abundance | 10 | 5 | 30 | 8 | 0 | 0 | 5 | 0 | 0 | 15 | 5 | 0 | 0 | 15 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
459.75 | 39-356-32-3,75 | 0 | 0 | 0 | Maestrichtian | MARLY CALC CHALK | Dominat lithology; numerical abundance | 25 | 5 | 25 | 8 | 0 | 0 | 0 | 0 | 0 | 8 | 5 | 0 | 0 | 15 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
462.24 | 39-356-32-5,24 | 0 | 0 | 0 | Maestrichtian | MARLY CALC CHALK | Dominat lithology; relative abundance | 15 | 0 | 30 | 10 | 0 | 0 | 0 | 0 | 0 | 15 | 10 | 2 | 4 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
486.90 | 39-356-33-2,50 | 0 | 0 | 0 | Middle campanian | MARLY CALC CHALK | Dominat lithology; relative abundance | 15 | 5 | 25 | 10 | 0 | 0 | 0 | 0 | 2 | 15 | 5 | 0 | 5 | 15 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
490.00 | 39-356-33-4,60 | 0 | 0 | 0 | Middle campanian | MARLY CALC CHALK | Dominat lithology; relative abundance | 15 | 10 | 20 | 15 | 0 | 0 | 0 | 0 | 0 | 15 | 10 | 0 | 2 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
514.18 | 39-356-34-1,83 | 0 | 0 | 0 | Lower campanian | CALCAREOUS MUD | Dominat lithology; relative abundance | 10 | 8 | 15 | 5 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 0 | 2 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 0 |
516.90 | 39-356-34-3,55 | 0 | 0 | 0 | Lower campanian | INOCERAMUS | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
517.10 | 39-356-34-3,75 | 0 | 0 | 0 | Lower campanian | MARLY CALC CHALK | Dominat lithology; relative abundance | 25 | 8 | 25 | 5 | 0 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 2 | 20 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
542.24 | 39-356-35-1,24 | 0 | 0 | 0 | Upper santonian | GLAUC | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
542.25 | 39-356-35-1,25 | 0 | 0 | 0 | Upper santonian | MN-FE NODULE | 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 | 0 |
544.31 | 39-356-35-2,81 | 0 | 0 | 0 | Upper santonian | MUDSTONE | Dominat lithology; relative abundance | 0 | 2 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 4 | 4 | 5 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 4 | 5 | 0 |
545.60 | 39-356-35-3,60 | 0 | 0 | 0 | Upper santonian | DOLOMITIC MARLY CALC CHALK | Dominat lithology; relative abundance | 5 | 15 | 20 | 15 | 0 | 0 | 0 | 0 | 0 | 10 | 5 | 0 | 0 | 20 | 0 | 5 | 0 | 0 | 4 | 0 | 1 | 0 | 0 | 0 | 0 |
572.25 | 39-356-36-2,75 | 0 | 0 | 0 | Upper santonian | DOLO MARLY CALC CHALK | Dominat lithology; relative abundance | 20 | 15 | 15 | 15 | 0 | 0 | 0 | 0 | 0 | 10 | 5 | 2 | 0 | 15 | 0 | 5 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 |
601.35 | 39-356-37-21,100 | 0 | 0 | 0 | Middle santonian | MARLY CALC CHALK | Dominat lithology; numerical abundance | 15 | 10 | 25 | 10 | 0 | 0 | 0 | 0 | 0 | 8 | 5 | 0 | 0 | 20 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
647.00 | 39-356-38-11,100 | 0 | 0 | 0 | Lower santonian | MARLY CALC CHALK | Dominat lithology; relative abundance | 30 | 5 | 15 | 5 | 0 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 2 | 25 | 0 | 4 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 |
650.30 | 39-356-38-31,130 | 0 | 0 | 0 | Lower santonian | MARLY CALC CHALK | Dominat lithology; relative abundance | 20 | 10 | 15 | 8 | 0 | 0 | 0 | 0 | 0 | 10 | 5 | 0 | 5 | 20 | 2 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
675.90 | 39-356-39-11,140 | 0 | 0 | 0 | Lower senonian | CALC MUDSTONE | Dominat lithology; relative abundance | 10 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 20 | 0 | 0 | 30 | 0 | 4 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 |
675.93 | 39-356-39-11,143 | 0 | 0 | 0 | Lower senonian | ZEOL SILTSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 20 | 8 | 10 | 30 | 0 | 4 | 0 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 |
676.69 | 39-356-39-2,69 | 0 | 0 | 0 | Lower senonian | CALC MUDSTONE | Dominat lithology; relative abundance | 20 | 5 | 10 | 5 | 0 | 0 | 0 | 0 | 0 | 15 | 5 | 0 | 5 | 30 | 0 | 5 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
677.05 | 39-356-39-21,105 | 0 | 0 | 0 | Lower senonian | CALC MUDSTONE | Dominat lithology; relative abundance | 20 | 18 | 5 | 8 | 0 | 0 | 0 | 0 | 0 | 15 | 5 | 0 | 0 | 25 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
678.30 | 39-356-39-3,80 | 10 | 20 | 70 | Lower senonian | SILTY CLAYSTONE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 1 | 0 | 1 | 75 | 1 | 0 | 2 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 |
680.11 | 39-356-39-41,111 | 20 | 30 | 50 | Lower senonian | SANDY SILTY CLAYSTONE | Dominat lithology; numerical abundance | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 25 | 1 | 0 | 0 | 65 | 2 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
694.95 | 39-356-40-11,100 | 0 | 0 | 0 | Coniacian | CALC MUDSTONE | Dominat lithology; relative abundance | 10 | 0 | 10 | 8 | 0 | 0 | 0 | 0 | 0 | 15 | 10 | 2 | 0 | 40 | 0 | 5 | 0 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 |
697.54 | 39-356-40-3,59 | 10 | 30 | 60 | Middle turonian | SILTY MUDSTONE | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 1 | 0 | 0 | 85 | 3 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
697.56 | 39-356-40-3,61 | 0 | 0 | 0 | Middle turonian | LIMESTONE | Dominat 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 | 0 | 0 | 0 |
697.58 | 39-356-40-3,63 | 0 | 0 | 0 | Middle turonian | CALC MUDSTONE | Dominat lithology; numerical abundance | 20 | 5 | 10 | 5 | 0 | 0 | 0 | 0 | 0 | 10 | 5 | 0 | 0 | 40 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
697.76 | 39-356-40-3,81 | 0 | 0 | 0 | Middle turonian | TERRIGENOUS CALC MUDSTONE | Dominat lithology; numerical abundance | 35 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 |
699.07 | 39-356-40-4,62 | 10 | 30 | 60 | Middle turonian | MUDSTONE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 1 | 0 | 0 | 65 | 0 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 |
701.35 | 39-356-40-51,140 | 0 | 30 | 60 | Middle turonian | SILTY MUDSTONE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 0 | 0 | 85 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
704.82 | 39-356-41-2,32 | 0 | 0 | 0 | Middle turonian | DOLO CALC MUDSTONE | Dominat lithology; relative abundance | 20 | 20 | 10 | 5 | 0 | 0 | 0 | 0 | 0 | 10 | 5 | 0 | 0 | 20 | 2 | 8 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
704.90 | 39-356-41-2,40 | 0 | 0 | 0 | Middle turonian | MUDSTONE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 35 | 20 | 0 | 0 | 35 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
704.93 | 39-356-41-2,43 | 0 | 0 | 0 | Middle turonian | PYRITIFEROUS MUDSTONE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 10 | 0 | 0 | 30 | 0 | 35 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
708.10 | 39-356-41-4,60 | 0 | 0 | 0 | Middle turonian | CALCITE CRUST | 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 | 0 | 0 | 0 |
710.20 | 39-356-41-51,120 | 5 | 25 | 60 | Upper albian | LIMESTONE | Dominat lithology; numerical abundance | 85 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
713.50 | 39-356-42-11,100 | 0 | 0 | 0 | Upper albian | CALC MUDSTONE | Dominat lithology; relative abundance | 10 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 5 | 0 | 0 | 40 | 2 | 5 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
713.80 | 39-356-42-11,130 | 0 | 0 | 0 | Upper albian | REVRYSTALLIZED CARBONATE | Dominat lithology; relative abundance | 40 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
715.05 | 39-356-42-21,105 | 0 | 0 | 0 | Upper albian | MUDSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 15 | 0 | 7 | 40 | 4 | 5 | 0 | 0 | 4 | 4 | 0 | 2 | 0 | 0 | 0 |
717.65 | 39-356-42-4,65 | 0 | 0 | 0 | Upper albian | DOLO LIMESTONE | Dominat lithology; relative abundance | 70 | 20 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
723.60 | 39-356-43-11,120 | 0 | 0 | 0 | Upper albian | RECRYSTALLIZED LIMESTONE | Dominat lithology; numerical abundance | 35 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 5 | 0 | 0 | 15 | 5 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
724.65 | 39-356-43-2,75 | 0 | 0 | 0 | Upper albian | MARLY LIMESTONE | Dominat lithology; relative abundance | 50 | 10 | 2 | 5 | 0 | 0 | 0 | 0 | 0 | 10 | 5 | 0 | 2 | 20 | 2 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 |
730.09 | 39-356-43-6,19 | 0 | 0 | 0 | Upper albian | DOLO RECRYSTALLIZED LIMESTONE | Dominat lithology; relative abundance | 40 | 30 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 10 | 5 | 0 | 0 | 0 | 2 | 4 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
730.83 | 39-356-43-6,93 | 0 | 0 | 0 | Upper albian | LIMESTONE | Minor lithology; relative abundance | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
730.88 | 39-356-43-6,98 | 10 | 30 | 60 | Upper albian | QUARTZOSE LIMESTONE | Minor lithology; numerical abundance | 85 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 1 | 0 | 0 | 0 | 1 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
731.34 | 39-356-43-61,144 | 0 | 0 | 0 | Upper albian | MARLY DOLO LIMESTONE | Dominat lithology; relative abundance | 35 | 20 | 2 | 8 | 0 | 0 | 0 | 0 | 0 | 10 | 5 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
733.90 | 39-356-44-2,90 | 0 | 0 | 0 | Upper albian | MARLY DOLO LIMESTONE | Dominat lithology; relative abundance | 35 | 15 | 2 | 5 | 0 | 0 | 0 | 0 | 0 | 10 | 5 | 0 | 5 | 15 | 4 | 4 | 0 | 0 | 4 | 4 | 0 | 0 | 0 | 0 | 0 |
737.04 | 39-356-44-41,104 | 0 | 0 | 0 | Upper albian | MARLY DOLO LIMESTONE | Dominat lithology; relative abundance | 45 | 15 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 0 | 20 | 0 | 4 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 |