Hollister, Charles D; Ewing, John I (2005): Smear slide analysis of Hole 11-100 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230322
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
Kaneps, Ansis G; Worstell, Paula J; Wilcoxon, James A; Poag, C Wylie; Paulus, F J; Luterbacher, Hanspeter; Lancelot, Yves; Hathaway, James; Habib, Daniel; Hollister, Charles D; Ewing, John I (1972): Initial Reports of the Deep Sea Drilling Project 11. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XI, 1077 pp, https://doi.org/10.2973/dsdp.proc.11.1972
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 24.687800 * Longitude: -73.799700
Date/Time Start: 1970-04-20T00:00:00 * Date/Time End: 1970-04-20T00:00:00
Minimum DEPTH, sediment/rock: 204.30 m * Maximum DEPTH, sediment/rock: 321.95 m
Event(s):
11-100 * Latitude: 24.687800 * Longitude: -73.799700 * Date/Time: 1970-04-20T00:00:00 * Elevation: -5325.0 m * Penetration: 331 m * Recovery: 29.4 m * Location: North Atlantic/BASIN * Campaign: Leg11 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 13 cores; 93 m cored; 0 m drilled; 31.6 % 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 | Radiolarians | Rad | % | Smear slide analysis | ||
13 | Quartz | Qz | % | Smear slide analysis | ||
14 | Feldspar | Fsp | % | Smear slide analysis | ||
15 | Mica | Mica | % | Smear slide analysis | ||
16 | Clay minerals | Clay min | % | Smear slide analysis | ||
17 | Glauconite | Glt | % | Smear slide analysis | ||
18 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
19 | Iron | Fe | % | Smear slide analysis | ||
20 | Limonite | Lm | % | Smear slide analysis | ||
21 | Magnetite | Fe3O4 | % | Smear slide analysis | ||
22 | Rutile | Rt | % | Smear slide analysis | ||
23 | Olivine | Ol | % | Smear slide analysis | ||
24 | Volcanic glass | Volc glass | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1884 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 Qz [%] | 14 Fsp [%] | 15 Mica [%] | 16 Clay min [%] | 17 Glt [%] | 18 Py [%] | 19 Fe [%] | 20 Lm [%] | 21 Fe3O4 [%] | 22 Rt [%] | 23 Ol [%] | 24 Volc glass [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
204.30 | 11-100-1-11,130 | 10 | 10 | 85 | Mesozoic | NANNO OOZE | Dominat lithology; relative abundance | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
204.50 | 11-100-1-2,0 | 0 | 35 | 85 | Mesozoic | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 96 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
205.49 | 11-100-1-2,99 | 0 | 10 | 0 | Mesozoic | NANNO OOZE | Dominat lithology; relative abundance | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
205.63 | 11-100-1-21,113 | 0 | 10 | 35 | Mesozoic | CHALK | Minor lithology; numerical abundance | 0 | 96 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
206.00 | 11-100-1-3,0 | 0 | 10 | 85 | Mesozoic | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
206.14 | 11-100-1-3,14 | 0 | 10 | 85 | Mesozoic | NANNO OOZE | Dominat lithology; numerical abundance | 13 | 86 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
206.24 | 11-100-1-3,24 | 0 | 10 | 85 | Mesozoic | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
206.96 | 11-100-1-3,96 | 0 | 10 | 85 | Mesozoic | NANNO OOZE | Dominat lithology; relative abundance | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
207.50 | 11-100-1-4,0 | 0 | 35 | 85 | Mesozoic | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
208.34 | 11-100-1-4,84 | 0 | 0 | 85 | Mesozoic | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
208.63 | 11-100-1-41,113 | 0 | 10 | 85 | Mesozoic | CHERT | Minor lithology; numerical abundance | 0 | 92 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
209.00 | 11-100-1-5,0 | 0 | 10 | 0 | Mesozoic | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
209.25 | 11-100-1-5,25 | 0 | 0 | 0 | Mesozoic | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
209.59 | 11-100-1-5,59 | 0 | 0 | 85 | Mesozoic | ORGANIC DEBRIS | Minor lithology; numerical abundance | 0 | 96 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 |
210.60 | 11-100-1-CC,0 | 0 | 0 | 0 | Mesozoic | CALCEDONIC QUARTZ AND MATRIX OF NANNO PLANKTON CHALK | Dominat lithology; numerical abundance | 55 | 100 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
210.60 | 11-100-1-CC,0 | 0 | 0 | 0 | Mesozoic | CHERT | Minor lithology; relative abundance | 0 | 100 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
210.60 | 11-100-1-CC,0 | 35 | 0 | 10 | Mesozoic | CHERT | Minor lithology; relative abundance | 0 | 12 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
210.60 | 11-100-1-CC,0 | 60 | 35 | 10 | Mesozoic | LIMESTONE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
210.60 | 11-100-1-CC,0 | 60 | 60 | 60 | Mesozoic | NANNO OOZE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
210.60 | 11-100-1-CC,0 | 85 | 85 | 85 | Mesozoic | QUARTZOSE CHERT MATRIX AND QUARTOSE CHERT FROM LIMESTONE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
237.00 | 11-100-2-1,0 | 0 | 0 | 0 | Upper jurassic | LIMESTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
238.09 | 11-100-2-11,109 | 0 | 60 | 60 | Upper jurassic | LIMESTONE | Dominat lithology; relative abundance | 0 | 46 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
238.50 | 11-100-2-2,0 | 0 | 85 | 10 | Upper jurassic | LIMESTONE | Dominat lithology; relative abundance | 75 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
238.83 | 11-100-2-2,33 | 0 | 60 | 85 | Upper jurassic | LIMESTONE | Dominat lithology; relative abundance | 0 | 55 | 0 | 0 | 0 | 0 | 6 | 55 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 |
239.56 | 11-100-2-21,106 | 0 | 10 | 85 | Upper jurassic | LIMESTONE | Dominat lithology; numerical abundance | 0 | 66 | 0 | 0 | 0 | 0 | 0 | 33 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
240.00 | 11-100-2-3,0 | 35 | 35 | 60 | Upper jurassic | LIMESTONE | Dominat lithology; relative abundance | 0 | 12 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
240.43 | 11-100-2-3,43 | 0 | 35 | 85 | Upper jurassic | LIMESTONE | Dominat lithology; relative abundance | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
240.69 | 11-100-2-3,69 | 0 | 60 | 60 | Upper jurassic | LIMESTONE | Dominat lithology; relative abundance | 6 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 |
241.60 | 11-100-2-CC,0 | 10 | 35 | 85 | Upper jurassic | LIMESTONE | Dominat lithology; relative abundance | 6 | 55 | 0 | 0 | 6 | 0 | 0 | 23 | 0 | 0 | 6 | 0 | 0 | 6 | 0 | 0 |
247.41 | 11-100-3-11,141 | 0 | 35 | 85 | Upper jurassic | LIMESTONE | Dominat lithology; numerical abundance | 4 | 72 | 0 | 0 | 0 | 0 | 4 | 15 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 |
247.60 | 11-100-3-CC,0 | 0 | 0 | 0 | Upper jurassic | CHERTY LIMESTONE | Dominat lithology; numerical abundance | 0 | 100 | 0 | 0 | 6 | 0 | 6 | 55 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 |
247.60 | 11-100-3-CC,0 | 0 | 10 | 85 | Upper jurassic | LIMESTONE | Dominat lithology; relative abundance | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
259.25 | 11-100-4-1,25 | 35 | 60 | 60 | Upper jurassic | LIMESTONE TO CALCISILTITE | Dominat lithology; relative abundance | 55 | 46 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
260.02 | 11-100-4-11,102 | 10 | 35 | 85 | Upper jurassic | LIMESTONE | Dominat lithology; numerical abundance | 0 | 58 | 0 | 0 | 0 | 0 | 0 | 29 | 0 | 0 | 12 | 0 | 0 | 0 | 0 | 0 |
260.60 | 11-100-4-CC,0 | 10 | 60 | 60 | Upper jurassic | LIMESTONE | Dominat lithology; relative abundance | 55 | 0 | 0 | 0 | 6 | 0 | 0 | 55 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 |
260.60 | 11-100-4-CC,0 | 10 | 85 | 60 | Upper jurassic | LIMESTONE | Minor lithology; relative abundance | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 |
262.19 | 11-100-5-11,119 | 0 | 10 | 85 | Upper jurassic | CALCILUTITE | Dominat lithology; relative abundance | 23 | 12 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
262.31 | 11-100-5-11,131 | 0 | 10 | 85 | Upper jurassic | CALCILUTITE | Dominat lithology; relative abundance | 55 | 12 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
262.67 | 11-100-5-2,17 | 0 | 10 | 85 | Upper jurassic | CALCILUTITE | Dominat lithology; relative abundance | 75 | 12 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
263.02 | 11-100-5-2,52 | 0 | 10 | 85 | Upper jurassic | CALCILUTITE | Dominat lithology; relative abundance | 75 | 12 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
263.53 | 11-100-5-21,103 | 0 | 10 | 85 | Upper jurassic | CALCILUTITE | Dominat lithology; relative abundance | 55 | 12 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 |
264.10 | 11-100-5-CC,0 | 10 | 35 | 60 | Upper jurassic | CALCILUTITE | Dominat lithology; numerical abundance | 12 | 42 | 0 | 0 | 3 | 0 | 0 | 30 | 0 | 0 | 12 | 0 | 0 | 0 | 0 | 0 |
267.60 | 11-100-6-1,60 | 0 | 10 | 85 | Upper jurassic | CALCILUTITE | Dominat lithology; numerical abundance | 12 | 56 | 0 | 0 | 0 | 0 | 0 | 28 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 |
268.39 | 11-100-6-11,139 | 0 | 10 | 85 | Upper jurassic | CALCILUTITE | Dominat lithology; numerical abundance | 30 | 60 | 0 | 0 | 3 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
270.10 | 11-100-6-CC,0 | 0 | 10 | 60 | Upper jurassic | CALCILUTITE | Dominat lithology; numerical abundance | 12 | 100 | 0 | 0 | 6 | 0 | 3 | 23 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 |
270.10 | 11-100-6-CC,0 | 0 | 35 | 60 | Upper jurassic | CALCILUTITE | Dominat lithology; numerical abundance | 30 | 29 | 0 | 0 | 0 | 0 | 0 | 29 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 |
270.10 | 11-100-6-CC,0 | 0 | 60 | 60 | Upper jurassic | CALCILUTITE | Dominat lithology; relative abundance | 6 | 46 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
270.10 | 11-100-6-CC,0 | 10 | 60 | 85 | Upper jurassic | CALCILUTITE | Minor lithology; relative abundance | 6 | 58 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
270.10 | 11-100-6-CC,0 | 10 | 60 | 85 | Upper jurassic | CALCISILTITE | Minor lithology; relative abundance | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
276.00 | 11-100-7-1,0 | 0 | 35 | 85 | Upper jurassic | LIMESTONE | Dominat lithology; relative abundance | 6 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
276.48 | 11-100-7-1,48 | 0 | 85 | 35 | Oxfordian | LIMESTONE | Dominat lithology; relative abundance | 6 | 61 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
276.90 | 11-100-7-1,90 | 35 | 10 | 60 | Oxfordian | LIMESTONE | Dominat lithology; relative abundance | 75 | 12 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
277.02 | 11-100-7-11,102 | 0 | 35 | 85 | Oxfordian | LIMESTONE | Dominat lithology; relative abundance | 0 | 100 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
277.31 | 11-100-7-11,131 | 0 | 35 | 85 | Oxfordian | CARBONACEOUS DEBRIS | Minor lithology; relative abundance | 55 | 61 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
277.50 | 11-100-7-2,0 | 0 | 10 | 85 | Oxfordian | CALCILUTITE | Dominat lithology; relative abundance | 75 | 12 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
277.69 | 11-100-7-2,19 | 0 | 10 | 85 | Oxfordian | CALCILUTITE | Dominat lithology; relative abundance | 75 | 29 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
278.53 | 11-100-7-21,103 | 0 | 10 | 85 | Oxfordian | CALCILUTITE | Dominat lithology; relative abundance | 75 | 12 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
279.10 | 11-100-7-CC,0 | 0 | 10 | 85 | Oxfordian | LIMESTONE | Dominat lithology; relative abundance | 55 | 61 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
286.00 | 11-100-8-1,0 | 0 | 10 | 85 | Oxfordian | CALCILUTITE | Dominat lithology; relative abundance | 75 | 12 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 23 | 6 | 0 | 0 | 0 | 0 | 0 |
287.14 | 11-100-8-11,114 | 0 | 10 | 85 | Jurassic | CALCILUTITE | Dominat lithology; relative abundance | 75 | 12 | 0 | 0 | 0 | 0 | 6 | 6 | 0 | 6 | 6 | 0 | 0 | 0 | 0 | 0 |
287.50 | 11-100-8-2,0 | 0 | 10 | 85 | Jurassic | CALCILUTITE | Dominat lithology; relative abundance | 75 | 29 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 6 | 6 | 0 | 0 | 0 | 0 | 0 |
288.60 | 11-100-8-21,110 | 0 | 10 | 85 | Jurassic | CALCILUTITE | Dominat lithology; relative abundance | 75 | 12 | 0 | 0 | 0 | 0 | 6 | 6 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 |
289.00 | 11-100-8-3,0 | 0 | 10 | 85 | Jurassic | CALCILUTITE | Dominat lithology; relative abundance | 75 | 12 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 6 | 6 | 0 | 0 | 0 | 0 | 0 |
289.96 | 11-100-8-3,96 | 0 | 10 | 85 | Jurassic | CALCILUTITE | Dominat lithology; relative abundance | 75 | 12 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 |
302.00 | 11-100-9-1,0 | 0 | 10 | 85 | Jurassic | CALCILUTITE | Dominat lithology; relative abundance | 75 | 12 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 |
302.93 | 11-100-9-1,93 | 0 | 10 | 85 | Jurassic | CALCILUTITE | Dominat lithology; relative abundance | 0 | 12 | 0 | 0 | 0 | 0 | 6 | 6 | 0 | 6 | 6 | 0 | 0 | 0 | 0 | 0 |
303.26 | 11-100-9-11,126 | 0 | 35 | 60 | Jurassic | CALCILUTITE TO CALCISILTITE | Dominat lithology; relative abundance | 55 | 61 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
303.50 | 11-100-9-2,0 | 10 | 10 | 85 | Jurassic | CALCILUTITE | Dominat lithology; relative abundance | 75 | 6 | 6 | 0 | 0 | 0 | 6 | 6 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 |
304.24 | 11-100-9-2,74 | 0 | 10 | 85 | Jurassic | CALCILUTITE | Dominat lithology; relative abundance | 55 | 29 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
304.64 | 11-100-9-21,114 | 0 | 10 | 85 | Jurassic | CALCILUTITE | Dominat lithology; relative abundance | 55 | 12 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
311.00 | 11-100-10-1,0 | 0 | 35 | 85 | Jurassic | CALCILUTITE | Dominat lithology; relative abundance | 75 | 12 | 0 | 0 | 0 | 0 | 6 | 6 | 6 | 0 | 6 | 0 | 0 | 0 | 0 | 0 |
311.82 | 11-100-10-1,82 | 0 | 10 | 85 | Jurassic | CALCILUTITE | Dominat lithology; relative abundance | 23 | 12 | 0 | 0 | 0 | 0 | 6 | 6 | 0 | 0 | 6 | 6 | 0 | 0 | 0 | 0 |
312.00 | 11-100-10-11,100 | 0 | 10 | 85 | Jurassic | CALCISILTITE | Minor lithology; relative abundance | 55 | 61 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 6 | 0 | 0 | 0 | 0 |
312.38 | 11-100-10-11,138 | 0 | 10 | 85 | Jurassic | CALCILUTITE | Dominat lithology; relative abundance | 23 | 61 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
312.50 | 11-100-10-2,0 | 0 | 10 | 85 | Jurassic | CALCILUTITE | Dominat lithology; relative abundance | 75 | 12 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
313.30 | 11-100-10-2,80 | 0 | 10 | 85 | Jurassic | CALCILUTITE | Dominat lithology; relative abundance | 55 | 12 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 |
313.78 | 11-100-10-21,128 | 0 | 10 | 85 | Jurassic | CALCILUTITE | Dominat lithology; relative abundance | 75 | 12 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
317.47 | 11-100-11-1,47 | 0 | 35 | 85 | Jurassic | MICRITIC LIMESTONE | Minor lithology; relative abundance | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
317.57 | 11-100-11-1,57 | 35 | 60 | 60 | Jurassic | BASALT | Dominat lithology; relative abundance | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 |
321.00 | 11-100-12-1,0 | 0 | 0 | 0 | Jurassic | FIBROUS CALCITE | Minor lithology; relative abundance | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
321.95 | 11-100-12-1,94 | 0 | 0 | 0 | BASALT | Dominat lithology; numerical abundance | 1 | 0 | 0 | 0 | 0 | 28 | 0 | 0 | 0 | 0 | 0 | 0 | 28 | 0 | 3 | 28 | |
321.95 | 11-100-12-1,94 | 0 | 0 | 0 | LIMESTONE | Minor lithology; relative abundance | 14 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |