Tucholke, Brian E; Vogt, Peter R (2005): Smear slide analysis of Hole 43-387 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230723
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
McCave, I Nick; Demars, Kenneth R; Kendrick, J W; Okada, Hisatake; McNulty, C L; Kaneps, Ansis G; Galehouse, J S; Houghton, R L; Rothe, Peter; Murdmaa, Ivar O; Tucholke, Brian E; Vogt, Peter R (1979): Initial Reports of the Deep Sea Drilling Project. U. S. Government Printing Office, XLIII, 1115 pp, https://doi.org/10.2973/dsdp.proc.43.1979
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 32.320000 * Longitude: -67.666700
Date/Time Start: 1975-08-01T00:00:00 * Date/Time End: 1975-08-01T00:00:00
Minimum DEPTH, sediment/rock: 32.70 m * Maximum DEPTH, sediment/rock: 789.80 m
Event(s):
43-387 * Latitude: 32.320000 * Longitude: -67.666700 * Date/Time: 1975-08-01T00:00:00 * Elevation: -5117.0 m * Penetration: 794.5 m * Recovery: 177.2 m * Location: North Atlantic/CONT RISE * Campaign: Leg43 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 50 cores; 468 m cored; 0 m drilled; 37.9 % 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 | Radiolarians | Rad | % | Smear slide analysis | ||
14 | Diatoms | Diatoms | % | Smear slide analysis | ||
15 | Spiculae | Spiculae | % | Smear slide analysis | ||
16 | Minerals, other | Min other | % | Smear slide analysis | ||
17 | Siderite | Sd | % | 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 | Biotite | Bt | % | Smear slide analysis | ||
23 | Clay minerals | Clay min | % | Smear slide analysis | ||
24 | Glauconite | Glt | % | Smear slide analysis | ||
25 | Opaque minerals | Opaque | % | Smear slide analysis | ||
26 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
27 | Iron | Fe | % | Smear slide analysis | ||
28 | Heavy minerals | HM | % | Smear slide analysis | ||
29 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
30 | Palagonite | Palagonite | % | Smear slide analysis | ||
31 | Organic matter | OM | % | Smear slide analysis | organic debris | |
32 | Terrigenous | Terr | % | Smear slide analysis | terrigeneous detritus |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
5886 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 Rad [%] | 14 Diatoms [%] | 15 Spiculae [%] | 16 Min other [%] | 17 Sd [%] | 18 Qz [%] | 19 Fsp [%] | 20 Zeo [%] | 21 Mica [%] | 22 Bt [%] | 23 Clay min [%] | 24 Glt [%] | 25 Opaque [%] | 26 Py [%] | 27 Fe [%] | 28 HM [%] | 29 Volc glass [%] | 30 Palagonite [%] | 31 OM [%] | 32 Terr [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
32.70 | 43-387-1-1,90 | 2 | 18 | 80 | Quaternary | CALCAREOUS CLAY | Dominat lithology; relative abundance | 0 | 0 | 11 | 8 | 0 | 0 | 0 | 2 | 0 | 2 | 2 | 1 | 0 | 0 | 78 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
34.05 | 43-387-1-2,75 | 0 | 20 | 80 | Quaternary | ZEOLITIC ? CLAY | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 20 | 0 | 0 | 76 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
35.55 | 43-387-1-3,75 | 0 | 20 | 80 | Quaternary | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 5 | 0 | 2 | 2 | 10 | 0 | 0 | 82 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
37.05 | 43-387-1-4,75 | 0 | 18 | 82 | Quaternary | ZEOLITIC ? CLAY | Dominat lithology; relative abundance | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 2 | 2 | 15 | 0 | 0 | 82 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
38.55 | 43-387-1-5,75 | 0 | 18 | 82 | Quaternary | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 5 | 0 | 2 | 8 | 0 | 0 | 0 | 5 | 0 | 0 | 82 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
40.05 | 43-387-1-6,75 | 0 | 20 | 80 | Quaternary | ZEOLITIC ? CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 2 | 0 | 20 | 0 | 2 | 78 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
100.75 | 43-387-2-2,75 | 0 | 18 | 82 | Oligocene | RAD MUD | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 15 | 2 | 1 | 1 | 2 | 0 | 0 | 2 | 0 | 0 | 82 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
102.25 | 43-387-2-3,75 | 0 | 13 | 87 | Oligocene | RAD MUD | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 10 | 0 | 2 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 87 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
103.75 | 43-387-2-4,75 | 0 | 12 | 88 | Oligocene | RAD MUD | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 10 | 0 | 2 | 1 | 0 | 0 | 2 | 1 | 0 | 0 | 88 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
105.25 | 43-387-2-5,75 | 0 | 12 | 88 | Oligocene | RAD MUD | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 10 | 2 | 2 | 1 | 0 | 2 | 2 | 1 | 0 | 0 | 88 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
137.35 | 43-387-3-1,75 | 0 | 15 | 85 | Upper eocene | RAD MUD | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 12 | 2 | 2 | 2 | 0 | 2 | 2 | 1 | 0 | 0 | 85 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
137.66 | 43-387-3-11,106 | 0 | 15 | 85 | Upper eocene | CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 3 | 2 | 2 | 12 | 0 | 0 | 0 | 1 | 0 | 0 | 85 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
139.40 | 43-387-3-21,130 | 0 | 23 | 87 | Upper eocene | RAD MUD | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 20 | 2 | 1 | 2 | 0 | 2 | 2 | 0 | 0 | 0 | 76 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
146.85 | 43-387-4-1,75 | 0 | 21 | 79 | Middle eocene | RAD MUD | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 15 | 2 | 3 | 0 | 0 | 2 | 2 | 3 | 2 | 0 | 79 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
155.78 | 43-387-5-CC,18 | 0 | 18 | 82 | Middle eocene | RAD MUD | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 17 | 2 | 1 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 82 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 82 |
168.29 | 43-387-6-3,19 | 0 | 15 | 85 | Middle eocene | RAD MUD | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 15 | 2 | 2 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 85 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 85 |
169.44 | 43-387-6-31,134 | 0 | 28 | 72 | Middle eocene | RAD MUD | Dominat lithology; relative abundance | 1 | 0 | 0 | 0 | 27 | 2 | 2 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 72 | 0 | 0 | 0 | 0 | 2 | 2 | 2 | 0 | 73 |
169.70 | 43-387-6-CC,10 | 0 | 25 | 75 | Middle eocene | RAD MUD | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 25 | 2 | 2 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 75 |
174.80 | 43-387-7-0,20 | 0 | 30 | 70 | Middle eocene | RAD MUD | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 27 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 70 | 2 | 1 | 0 | 0 | 2 | 1 | 2 | 0 | 72 |
175.43 | 43-387-7-1,48 | 0 | 19 | 81 | Middle eocene | RAD MUD | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 18 | 2 | 1 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 81 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 81 |
175.70 | 43-387-7-1,75 | 0 | 28 | 72 | Middle eocene | RAD MUD | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 28 | 2 | 2 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 72 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 72 |
176.25 | 43-387-7-11,130 | 0 | 30 | 70 | Middle eocene | RAD MUD | Dominat lithology; relative abundance | 1 | 0 | 0 | 0 | 28 | 2 | 1 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 70 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 71 |
177.20 | 43-387-7-2,75 | 0 | 35 | 65 | Middle eocene | RAD MUD | Dominat lithology; relative abundance | 0 | 0 | 2 | 0 | 32 | 2 | 3 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 63 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 63 |
177.23 | 43-387-7-2,78 | 0 | 40 | 60 | Middle eocene | PYRITE SILICEOUS MUD | Minor lithology; relative abundance | 2 | 0 | 0 | 0 | 8 | 2 | 10 | 0 | 0 | 1 | 3 | 0 | 1 | 0 | 56 | 1 | 0 | 0 | 20 | 0 | 0 | 2 | 0 | 0 |
178.05 | 43-387-7-3,10 | 0 | 30 | 70 | Middle eocene | RAD MUD | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 30 | 2 | 5 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 65 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 65 |
178.70 | 43-387-7-3,75 | 0 | 60 | 30 | Middle eocene | RAD OOZE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 55 | 2 | 5 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 29 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 |
180.20 | 43-387-7-4,75 | 0 | 55 | 45 | Middle eocene | RAD OOZE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 5 | 2 | 7 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 43 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 43 |
181.48 | 43-387-7-5,53 | 0 | 50 | 50 | Middle eocene | RAD MUD | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 42 | 2 | 3 | 0 | 0 | 1 | 2 | 0 | 1 | 0 | 48 | 2 | 0 | 0 | 0 | 0 | 2 | 1 | 0 | 55 |
182.64 | 43-387-7-6,19 | 0 | 45 | 50 | Middle eocene | SPONGE SPICULE MUD | Minor lithology; numerical abundance | 2 | 0 | 0 | 0 | 4 | 0 | 20 | 0 | 0 | 2 | 2 | 0 | 1 | 0 | 50 | 6 | 2 | 0 | 0 | 0 | 4 | 0 | 0 | 74 |
183.99 | 43-387-7-CC,4 | 0 | 35 | 65 | Middle eocene | RAD MUD | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 32 | 2 | 3 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 65 | 2 | 2 | 0 | 0 | 2 | 0 | 2 | 0 | 65 |
185.10 | 43-387-8-1,90 | 1 | 45 | 55 | Middle eocene | RAD MUD | Dominat lithology; relative abundance | 1 | 0 | 0 | 0 | 40 | 2 | 7 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 51 | 1 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 53 |
185.50 | 43-387-8-11,130 | 0 | 40 | 60 | Middle eocene | CALCAREOUS RAD MUD | Dominat lithology; relative abundance | 11 | 0 | 5 | 0 | 38 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 44 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 57 |
185.85 | 43-387-8-2,15 | 0 | 45 | 55 | Middle eocene | NANNO RAD MUD | Dominat lithology; relative abundance | 2 | 0 | 18 | 0 | 22 | 2 | 2 | 0 | 0 | 2 | 1 | 0 | 2 | 0 | 54 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 56 |
187.05 | 43-387-8-21,135 | 0 | 35 | 65 | Middle eocene | RAD MUD | Dominat lithology; relative abundance | 1 | 0 | 12 | 2 | 18 | 0 | 3 | 0 | 0 | 2 | 1 | 0 | 2 | 0 | 64 | 1 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 61 |
187.28 | 43-387-8-CC,8 | 0 | 28 | 72 | Middle eocene | RAD MUD | Dominat lithology; relative abundance | 2 | 0 | 1 | 0 | 25 | 2 | 1 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 71 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 73 |
193.89 | 43-387-9-0,19 | 1 | 39 | 60 | Middle eocene | NANNO RAD MUD | Minor lithology; relative abundance | 3 | 0 | 16 | 2 | 24 | 1 | 2 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 54 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 57 |
194.00 | 43-387-9-0,30 | 4 | 31 | 65 | Middle eocene | RAD MUD | Dominat lithology; relative abundance | 10 | 0 | 3 | 2 | 26 | 1 | 5 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 55 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 65 |
194.50 | 43-387-9-1,40 | 2 | 38 | 60 | Middle eocene | CALCAREOUS RAD MUD | Dominat lithology; relative abundance | 12 | 0 | 0 | 0 | 26 | 2 | 3 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 56 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 65 |
195.30 | 43-387-9-11,120 | 0 | 35 | 65 | Middle eocene | NANNO RAD MUD | Dominat lithology; relative abundance | 2 | 0 | 18 | 0 | 13 | 2 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 65 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 65 |
196.00 | 43-387-9-2,40 | 5 | 30 | 65 | Middle eocene | RAD MUD | Dominat lithology; relative abundance | 1 | 0 | 2 | 0 | 30 | 2 | 3 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 64 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 65 |
197.28 | 43-387-9-3,18 | 2 | 33 | 65 | Middle eocene | NANNO RAD MUD | Dominat lithology; relative abundance | 2 | 0 | 16 | 2 | 12 | 2 | 2 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 59 | 2 | 1 | 0 | 0 | 0 | 1 | 1 | 0 | 79 |
199.35 | 43-387-9-4,75 | 1 | 34 | 65 | Middle eocene | NANNO RAD MUD | Dominat lithology; relative abundance | 3 | 0 | 19 | 0 | 16 | 2 | 2 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 58 | 2 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 67 |
200.85 | 43-387-9-5,75 | 0 | 34 | 66 | Middle eocene | NANNO RAD MUD | Dominat lithology; relative abundance | 1 | 0 | 15 | 0 | 16 | 2 | 2 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 66 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 62 |
202.35 | 43-387-9-6,75 | 5 | 40 | 55 | Middle eocene | SPONGE SPICULE RAD MUD OR SILICEOUS MUD | Dominat lithology; relative abundance | 6 | 0 | 5 | 0 | 25 | 2 | 15 | 0 | 0 | 2 | 1 | 0 | 2 | 0 | 47 | 1 | 2 | 0 | 0 | 2 | 0 | 2 | 0 | 55 |
202.90 | 43-387-9-61,130 | 2 | 33 | 65 | Middle eocene | RAD MUD | Dominat lithology; relative abundance | 3 | 0 | 8 | 2 | 18 | 2 | 4 | 0 | 0 | 2 | 2 | 0 | 1 | 0 | 60 | 1 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 64 |
203.20 | 43-387-9-CC,0 | 5 | 35 | 60 | Middle eocene | RAD MUD | Dominat lithology; relative abundance | 2 | 0 | 11 | 2 | 25 | 2 | 4 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 57 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 |
203.40 | 43-387-10-0,20 | 2 | 33 | 65 | Middle eocene | MUDDY RAD OOZE | Dominat lithology; relative abundance | 2 | 0 | 4 | 2 | 40 | 1 | 14 | 0 | 0 | 2 | 1 | 0 | 2 | 0 | 38 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 57 |
204.69 | 43-387-10-11,109 | 2 | 43 | 55 | Middle eocene | MUDDY RAD OOZE | Dominat lithology; relative abundance | 2 | 0 | 6 | 2 | 40 | 1 | 6 | 0 | 0 | 2 | 2 | 0 | 1 | 0 | 41 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 52 |
205.51 | 43-387-10-2,41 | 0 | 30 | 70 | Middle eocene | CALCAREOUS MUDDY RAD OOZE | Dominat lithology; relative abundance | 10 | 0 | 12 | 0 | 24 | 4 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 48 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
207.40 | 43-387-10-3,80 | 1 | 29 | 60 | Middle eocene | MUDDY RAD OOZE | Dominat lithology; relative abundance | 2 | 0 | 1 | 0 | 40 | 2 | 8 | 0 | 0 | 2 | 1 | 2 | 2 | 0 | 47 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 60 |
208.36 | 43-387-10-4,26 | 6 | 39 | 55 | Middle eocene | MUDDY RAD OOZE | Dominat lithology; relative abundance | 2 | 0 | 8 | 2 | 45 | 2 | 2 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 40 | 0 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | 51 |
209.83 | 43-387-10-5,23 | 2 | 33 | 65 | Middle eocene | RAD MUD | Dominat lithology; relative abundance | 2 | 0 | 2 | 0 | 40 | 1 | 5 | 0 | 0 | 2 | 1 | 0 | 2 | 0 | 50 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 67 |
211.60 | 43-387-10-6,50 | 2 | 38 | 60 | Middle eocene | MUDDY RAD OOZE | Dominat lithology; relative abundance | 2 | 0 | 2 | 0 | 4 | 2 | 8 | 0 | 0 | 2 | 1 | 0 | 2 | 0 | 45 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 59 |
212.70 | 43-387-10-CC,0 | 1 | 39 | 60 | Middle eocene | RAD MUD | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 30 | 1 | 6 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 58 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 63 |
214.25 | 43-387-11-11,145 | 5 | 45 | 50 | Middle eocene | MUDDY RAD OOZE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 50 | 1 | 1 | 0 | 0 | 2 | 1 | 0 | 2 | 0 | 47 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
223.44 | 43-387-12-11,114 | 5 | 50 | 45 | Middle eocene | MUDDY RAD OOZE | Dominat lithology; relative abundance | 1 | 0 | 1 | 0 | 45 | 1 | 5 | 1 | 0 | 1 | 2 | 0 | 0 | 0 | 43 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
232.91 | 43-387-13-11,111 | 0 | 24 | 76 | Middle eocene | CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 7 | 3 | 5 | 2 | 1 | 5 | 0 | 2 | 2 | 0 | 2 | 0 | 74 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
234.46 | 43-387-13-21,116 | 0 | 25 | 75 | Middle eocene | NANNO CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 20 | 3 | 3 | 2 | 2 | 5 | 0 | 2 | 2 | 0 | 0 | 0 | 66 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
234.78 | 43-387-13-21,148 | 0 | 20 | 80 | Middle eocene | NANNO CLAYSTONE | Dominat lithology; relative abundance | 4 | 0 | 15 | 1 | 2 | 0 | 0 | 5 | 0 | 2 | 4 | 0 | 0 | 0 | 74 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
242.76 | 43-387-14-11,146 | 0 | 60 | 40 | Middle eocene | CALCAREOUS MUDDY SILICEOUS OOZE | Dominat lithology; numerical abundance | 3 | 0 | 14 | 3 | 25 | 18 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 34 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
243.39 | 43-387-14-2,59 | 0 | 21 | 79 | Middle eocene | SILICIFIED CLAYSTONE | Dominat lithology; numerical abundance | 2 | 0 | 3 | 3 | 8 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 0 | 0 | 79 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
250.80 | 43-387-15-CC,0 | 0 | 21 | 79 | Middle eocene | SILICIFIED (RADS) CLAYSTONE OR RAD MUDSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 2 | 15 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 2 | 0 | 79 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
260.87 | 43-387-16-1,77 | 0 | 24 | 76 | Eocene | CALCAREOUS (SILICIFIED ?) CLAYSTONE | Dominat lithology; relative abundance | 10 | 0 | 7 | 2 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 76 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
261.21 | 43-387-16-11,111 | 0 | 21 | 79 | Eocene | SILICIFIED (RADS) CLAYSTONE OR RAD MUDSTONE | Dominat lithology; relative abundance | 7 | 0 | 2 | 2 | 15 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 72 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
262.35 | 43-387-16-2,75 | 0 | 22 | 78 | Eocene | CALCAREOUS SILICIFIED CLAYSTONE OR CALCAREOUS RAD MUDSTONE | Dominat lithology; relative abundance | 10 | 0 | 8 | 2 | 10 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 68 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
270.89 | 43-387-17-11,129 | 0 | 15 | 85 | Eocene | CALCAREOUS (SILICIFIED ?) CLAYSTONE | Dominat lithology; relative abundance | 14 | 0 | 2 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 81 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
289.10 | 43-387-18-1,40 | 0 | 4 | 96 | Lower eocene | SILICIFIED CLAYSTONE | Dominat lithology; relative abundance | 1 | 0 | 2 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 2 | 0 | 96 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 98 |
290.00 | 43-387-18-11,130 | 0 | 20 | 80 | Lower eocene | CALCAREOUS RAD MUDSTONE | Dominat lithology; numerical abundance | 20 | 0 | 2 | 1 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 66 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 87 |
290.30 | 43-387-18-CC,0 | 0 | 25 | 75 | Lower eocene | RAD MUDSTONE | Dominat lithology; relative abundance | 4 | 0 | 1 | 6 | 15 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 2 | 0 | 71 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 78 |
308.50 | 43-387-19-1,80 | 0 | 8 | 92 | Lower eocene | CLAYSTONE | Dominat lithology; relative abundance | 4 | 0 | 2 | 1 | 3 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 1 | 0 | 89 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 94 |
308.66 | 43-387-19-1,96 | 0 | 9 | 91 | Lower eocene | CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 1 | 2 | 7 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 1 | 0 | 91 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 92 |
309.75 | 43-387-19-2,55 | 5 | 35 | 60 | Lower eocene | SPONGE SPICULE MUDSTONE OR SILICEOUS MUDSTONE | Dominat lithology; relative abundance | 7 | 0 | 1 | 2 | 10 | 0 | 20 | 0 | 0 | 0 | 2 | 0 | 3 | 0 | 58 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 69 |
309.90 | 43-387-19-2,70 | 0 | 10 | 90 | Lower eocene | CALCAREOUS (SILICIFIED ?) CLAYSTONE | Dominat lithology; relative abundance | 22 | 0 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 71 | 2 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 93 |
311.84 | 43-387-19-31,114 | 0 | 13 | 87 | Lower eocene | CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 3 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 1 | 0 | 89 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 92 |
312.30 | 43-387-19-CC,0 | 0 | 43 | 57 | Lower eocene | SPONGE SPICULE MUDSTONE | Dominat lithology; relative abundance | 11 | 0 | 3 | 0 | 7 | 0 | 28 | 0 | 0 | 0 | 2 | 0 | 4 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 65 |
328.00 | 43-387-20-11,130 | 0 | 26 | 74 | Lower eocene | SILTY CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 2 | 2 | 2 | 2 | 1 | 0 | 0 | 2 | 1 | 0 | 10 | 0 | 74 | 4 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 92 |
328.76 | 43-387-20-2,56 | 0 | 20 | 80 | Lower eocene | RAD MUDSTONE | Dominat lithology; relative abundance | 5 | 0 | 6 | 0 | 12 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 1 | 0 | 76 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 81 |
330.84 | 43-387-20-31,114 | 3 | 22 | 75 | Lower eocene | NANNO CLAYSTONE | Dominat lithology; numerical abundance | 5 | 0 | 15 | 0 | 7 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 72 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 74 |
331.30 | 43-387-20-CC,0 | 0 | 12 | 88 | Lower eocene | CLAYSTONE | Dominat lithology; relative abundance | 4 | 0 | 8 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 88 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 92 |
346.55 | 43-387-21-1,85 | 7 | 28 | 65 | Lower eocene | RAD MUDSTONE | Dominat lithology; relative abundance | 5 | 0 | 9 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 54 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 66 |
346.81 | 43-387-21-11,111 | 3 | 32 | 65 | Lower eocene | RAD MUDSTONE | Dominat lithology; relative abundance | 2 | 0 | 1 | 0 | 32 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 1 | 0 | 64 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 67 |
346.84 | 43-387-21-11,114 | 3 | 27 | 70 | Lower eocene | CALCAREOUS RAD MUDSTONE | Dominat lithology; relative abundance | 5 | 0 | 10 | 0 | 20 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 60 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 72 |
347.91 | 43-387-21-2,71 | 0 | 12 | 88 | Lower eocene | CLACAREOUS CLAYSTONE | Dominat lithology; relative abundance | 12 | 0 | 12 | 2 | 7 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 69 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 90 |
356.81 | 43-387-22-2,11 | 1 | 44 | 55 | Lower eocene | MUDDY RAD OOZE (SILICIFIED) | Dominat lithology; relative abundance | 1 | 0 | 2 | 0 | 50 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 49 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 50 |
357.08 | 43-387-22-2,38 | 0 | 0 | 0 | Lower eocene | RAD MUDSTONE | Dominat lithology; relative abundance | 3 | 0 | 5 | 2 | 16 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 73 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
357.49 | 43-387-22-2,79 | 5 | 30 | 65 | Lower eocene | (SILICIFIED) FORAM RAD MUDSTONE | Dominat lithology; relative abundance | 5 | 0 | 2 | 17 | 10 | 2 | 2 | 0 | 0 | 0 | 1 | 0 | 2 | 0 | 65 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 68 |
358.87 | 43-387-22-3,67 | 0 | 35 | 65 | Lower eocene | NANNO RAD MUDSTONE | Dominat lithology; relative abundance | 6 | 0 | 15 | 0 | 28 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 49 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 64 |
375.08 | 43-387-23-1,78 | 0 | 10 | 90 | Lower eocene | CALCAREOUS CLAYSTONE | Dominat lithology; relative abundance | 10 | 0 | 12 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 2 | 0 | 77 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
376.44 | 43-387-23-2,64 | 0 | 1 | 99 | Lower eocene | SILICIFIED CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 2 | 0 | 100 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
378.28 | 43-387-23-3,98 | 0 | 9 | 91 | Lower eocene | CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 5 | 0 | 0 | 2 | 2 | 0 | 1 | 0 | 2 | 0 | 91 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
380.01 | 43-387-23-41,121 | 0 | 2 | 98 | Lower eocene | CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 1 | 0 | 2 | 0 | 98 | 2 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 |
380.38 | 43-387-23-5,8 | 0 | 10 | 90 | Lower eocene | CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 1 | 5 | 0 | 2 | 0 | 90 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
394.04 | 43-387-24-1,74 | 0 | 22 | 78 | Lower paleocene | CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 1 | 2 | 5 | 0 | 0 | 8 | 0 | 0 | 0 | 0 | 2 | 0 | 78 | 2 | 2 | 1 | 0 | 2 | 2 | 0 | 0 | 0 |
394.65 | 43-387-24-11,135 | 0 | 7 | 93 | Lower paleocene | CLAYSTONE | Dominat lithology; relative abundance | 6 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 89 | 1 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
394.90 | 43-387-24-CC,0 | 0 | 11 | 89 | Lower paleocene | CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 2 | 0 | 9 | 0 | 0 | 0 | 0 | 2 | 1 | 0 | 2 | 0 | 89 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
404.10 | 43-387-25-11,130 | 0 | 5 | 95 | Lower paleocene | CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 3 | 0 | 0 | 1 | 0 | 2 | 2 | 0 | 2 | 0 | 95 | 2 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
404.75 | 43-387-25-2,45 | 0 | 6 | 94 | Lower paleocene | CLAYSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 1 | 0 | 2 | 2 | 0 | 2 | 0 | 93 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
405.47 | 43-387-25-21,117 | 0 | 5 | 95 | Lower paleocene | CLAYSTONE | Dominat lithology; relative abundance | 3 | 0 | 6 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 2 | 0 | 89 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
405.95 | 43-387-25-3,15 | 0 | 3 | 97 | Lower paleocene | CLAYSTONE | Dominat lithology; relative abundance | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 2 | 0 | 96 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
412.59 | 43-387-26-1,39 | 0 | 14 | 86 | Lower paleocene | CLAYSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 3 | 0 | 2 | 5 | 0 | 2 | 0 | 86 | 1 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 |
413.98 | 43-387-26-2,28 | 0 | 4 | 96 | Lower paleocene | CLAYSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 2 | 1 | 0 | 2 | 0 | 96 | 2 | 2 | 0 | 0 | 2 | 2 | 0 | 0 | 0 |
415.55 | 43-387-26-3,35 | 0 | 3 | 97 | Lower paleocene | CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 2 | 1 | 0 | 2 | 0 | 97 | 2 | 2 | 0 | 0 | 2 | 2 | 0 | 0 | 0 |
442.10 | 43-387-27-1,85 | 0 | 16 | 84 | CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 10 | 0 | 0 | 0 | 84 | 2 | 1 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | |
442.53 | 43-387-27-11,128 | 5 | 23 | 72 | SILTY CLAYSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 5 | 14 | 0 | 5 | 0 | 72 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | |
443.05 | 43-387-27-2,30 | 0 | 26 | 74 | SILTY CLAYSTONE | Minor lithology; relative abundance | 2 | 0 | 2 | 0 | 9 | 0 | 0 | 5 | 0 | 2 | 7 | 0 | 1 | 0 | 74 | 0 | 1 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | |
443.11 | 43-387-27-2,36 | 0 | 3 | 97 | CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 2 | 0 | 2 | 0 | 97 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | |
445.00 | 43-387-27-3,75 | 0 | 20 | 80 | Upper cretaceous | CALCAREOUS CLAYSTONE | Dominat lithology; relative abundance | 25 | 0 | 10 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 63 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
446.50 | 43-387-27-4,75 | 0 | 40 | 60 | Upper cretaceous | MARLY CHALK | Dominat lithology; relative abundance | 30 | 0 | 10 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
448.00 | 43-387-27-5,75 | 0 | 25 | 75 | Upper cretaceous | MARLY CHALK | Dominat lithology; relative abundance | 30 | 0 | 10 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 58 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
449.50 | 43-387-27-6,75 | 0 | 20 | 80 | Upper cretaceous | MARLY CHALK | Dominat lithology; relative abundance | 30 | 0 | 10 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 57 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
461.10 | 43-387-28-11,120 | 0 | 20 | 80 | Upper cretaceous | MARLY CHALK | Dominat lithology; relative abundance | 20 | 0 | 10 | 7 | 0 | 0 | 0 | 0 | 2 | 2 | 2 | 0 | 2 | 0 | 67 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
471.55 | 43-387-29-2,65 | 0 | 6 | 94 | Upper cretaceous | CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 94 | 2 | 1 | 0 | 0 | 2 | 1 | 2 | 0 | 98 |
473.25 | 43-387-29-3,85 | 0 | 8 | 92 | Upper cretaceous | CLAYSTONE | Dominat lithology; relative abundance | 1 | 0 | 2 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 92 | 1 | 2 | 0 | 0 | 2 | 3 | 0 | 0 | 98 |
474.95 | 43-387-29-41,105 | 0 | 15 | 85 | Upper cretaceous | CLAYSTONE | Minor lithology; relative abundance | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 1 | 3 | 2 | 1 | 0 | 85 | 0 | 0 | 0 | 0 | 0 | 10 | 2 | 0 | 100 |
475.50 | 43-387-29-CC,0 | 0 | 12 | 88 | Upper cretaceous | CLAYSTONE | Dominat lithology; relative abundance | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 2 | 0 | 88 | 0 | 0 | 0 | 0 | 2 | 1 | 2 | 0 | 100 |
489.45 | 43-387-30-1,95 | 0 | 10 | 90 | Upper cretaceous | CLAYSTONE | Dominat lithology; relative abundance | 1 | 0 | 0 | 0 | 7 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | 87 | 0 | 0 | 0 | 0 | 2 | 2 | 2 | 0 | 100 |
489.59 | 43-387-30-11,109 | 2 | 73 | 25 | Upper cretaceous | RAD OOZE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 75 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 25 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
489.83 | 43-387-30-11,133 | 15 | 60 | 25 | Upper cretaceous | CARBONACEOUS RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 25 | 0 | 0 | 5 | 0 | 2 | 0 | 0 | 15 | 30 |
490.10 | 43-387-30-CC,0 | 0 | 32 | 68 | Upper cretaceous | RAD MUDSTONE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 30 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 68 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 70 |
508.40 | 43-387-31-1,90 | 0 | 9 | 91 | Upper cretaceous | CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 | 91 | 0 | 1 | 0 | 0 | 2 | 1 | 2 | 0 | 98 |
508.65 | 43-387-31-11,115 | 0 | 9 | 91 | Upper cretaceous | CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 | 91 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 0 | 100 |
509.10 | 43-387-31-CC,0 | 0 | 0 | 0 | Upper cretaceous | CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 2 | 0 | 97 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 0 |
517.35 | 43-387-32-0,25 | 0 | 8 | 92 | Cretaceous | CLAYSTONE | Dominat lithology; relative abundance | 1 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 5 | 0 | 92 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 100 |
518.01 | 43-387-32-1,55 | 0 | 9 | 91 | Cretaceous | CLAYSTONE | Dominat lithology; relative abundance | 1 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 5 | 0 | 91 | 0 | 0 | 0 | 0 | 2 | 1 | 1 | 0 | 100 |
519.76 | 43-387-32-2,80 | 0 | 12 | 88 | Cretaceous | CLAYSTONE | Dominat lithology; relative abundance | 1 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 6 | 0 | 88 | 0 | 1 | 2 | 0 | 1 | 0 | 1 | 0 | 100 |
521.65 | 43-387-32-31,119 | 0 | 10 | 90 | Cretaceous | CLAYSTONE | Dominat lithology; relative abundance | 1 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 3 | 0 | 90 | 2 | 1 | 0 | 0 | 0 | 2 | 1 | 0 | 96 |
522.55 | 43-387-32-4,59 | 0 | 25 | 75 | Cretaceous | CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 7 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 7 | 0 | 75 | 2 | 0 | 0 | 0 | 9 | 1 | 2 | 0 | 93 |
524.25 | 43-387-32-5,79 | 2 | 14 | 84 | Cretaceous | CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 5 | 0 | 84 | 2 | 1 | 0 | 0 | 2 | 1 | 2 | 0 | 94 |
525.97 | 43-387-32-61,101 | 0 | 65 | 35 | Cretaceous | MARLY CALCAREOUS OOZE OR MARLY CHALK | Minor lithology; relative abundance | 64 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 1 | 0 | 30 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
526.28 | 43-387-32-61,132 | 30 | 20 | 50 | Cretaceous | RAD MUDSTONE | Minor lithology; relative abundance | 5 | 0 | 0 | 0 | 35 | 0 | 1 | 0 | 0 | 0 | 2 | 2 | 3 | 0 | 48 | 0 | 0 | 7 | 0 | 1 | 2 | 0 | 23 | 64 |
527.95 | 43-387-33-11,135 | 0 | 12 | 88 | Cretaceous | CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 1 | 0 | 88 | 0 | 0 | 3 | 0 | 3 | 2 | 0 | 0 | 95 |
529.76 | 43-387-33-3,16 | 0 | 11 | 89 | Cretaceous | CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 2 | 0 | 8 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 3 | 0 | 89 | 2 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 |
531.20 | 43-387-33-CC,0 | 0 | 10 | 90 | Cretaceous | CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 90 | 0 | 0 | 2 | 0 | 2 | 2 | 2 | 0 | 94 |
537.35 | 43-387-34-11,115 | 0 | 15 | 85 | Lower cretaceous | CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 9 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 4 | 0 | 85 | 0 | 1 | 2 | 0 | 1 | 0 | 2 | 0 | 87 |
539.07 | 43-387-34-21,137 | 0 | 20 | 80 | Lower cretaceous | RAD MUDSTONE | Dominat lithology; relative abundance | 1 | 0 | 2 | 0 | 15 | 0 | 2 | 0 | 0 | 0 | 2 | 2 | 1 | 0 | 80 | 0 | 1 | 1 | 0 | 1 | 0 | 2 | 0 | 85 |
539.78 | 43-387-34-3,58 | 30 | 50 | 20 | Lower cretaceous | RAD OOZE | Minor lithology; relative abundance | 2 | 0 | 0 | 0 | 76 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 2 | 0 | 20 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 24 |
539.99 | 43-387-34-3,79 | 12 | 13 | 75 | Lower cretaceous | RAD MUDSTONE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 22 | 0 | 2 | 0 | 0 | 0 | 2 | 2 | 1 | 0 | 74 | 0 | 2 | 1 | 0 | 2 | 0 | 2 | 0 | 78 |
541.86 | 43-387-34-41,116 | 5 | 25 | 70 | Lower cretaceous | RADMUDSTONE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 24 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 3 | 0 | 70 | 0 | 2 | 1 | 0 | 2 | 0 | 0 | 0 | 76 |
542.30 | 43-387-34-CC,0 | 0 | 29 | 71 | Lower cretaceous | RAD MUDSTONE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 27 | 0 | 2 | 0 | 0 | 0 | 2 | 2 | 1 | 0 | 71 | 0 | 0 | 0 | 0 | 1 | 0 | 2 | 0 | 74 |
546.80 | 43-387-35-11,110 | 0 | 0 | 0 | Lower cretaceous | ALTERED AND RECRYSTALLIZED RADS | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
546.80 | 43-387-35-11,110 | 0 | 0 | 0 | Lower cretaceous | RAD SANDSTONE | Minor lithology; relative 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 |
547.83 | 43-387-35-2,63 | 0 | 20 | 80 | Lower cretaceous | RAD MUDSTONE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 15 | 0 | 0 | 2 | 0 | 2 | 2 | 0 | 1 | 0 | 78 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
549.51 | 43-387-35-3,81 | 0 | 12 | 88 | Lower cretaceous | RAD MUDSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 1 | 2 | 2 | 2 | 0 | 2 | 0 | 88 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
550.97 | 43-387-35-4,77 | 10 | 22 | 68 | Lower cretaceous | RAD MUDSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 25 | 0 | 0 | 2 | 0 | 1 | 1 | 0 | 1 | 0 | 68 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
551.00 | 43-387-35-4,80 | 2 | 16 | 82 | Lower cretaceous | RAD MUDSTONE | Dominat lithology; relative abundance | 1 | 0 | 0 | 0 | 10 | 0 | 0 | 2 | 2 | 1 | 1 | 0 | 1 | 0 | 82 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
552.55 | 43-387-35-5,85 | 0 | 10 | 90 | Lower cretaceous | CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 8 | 0 | 0 | 1 | 0 | 2 | 2 | 0 | 2 | 0 | 90 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
556.16 | 43-387-36-1,86 | 0 | 14 | 86 | Lower cretaceous | CLAYSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 9 | 0 | 0 | 2 | 0 | 2 | 1 | 0 | 1 | 0 | 86 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
557.30 | 43-387-36-2,50 | 0 | 12 | 88 | Lower cretaceous | CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 5 | 0 | 0 | 1 | 0 | 1 | 1 | 0 | 1 | 0 | 88 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
557.88 | 43-387-36-21,108 | 0 | 50 | 50 | Lower cretaceous | MARLY LIMESTONE (CHALK ?) | Minor lithology; relative abundance | 50 | 0 | 0 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 48 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
559.45 | 43-387-36-31,115 | 0 | 15 | 85 | Lower cretaceous | CLAYSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 8 | 0 | 0 | 2 | 0 | 2 | 1 | 0 | 2 | 0 | 86 | 0 | 3 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
560.24 | 43-387-36-4,44 | 55 | 35 | 10 | Lower cretaceous | RAD CALCAREOUS SILTY SANDSTONE (RAD LIMESTONE) | Minor lithology; relative abundance | 48 | 0 | 0 | 2 | 38 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 1 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
575.26 | 43-387-37-1,96 | 0 | 23 | 77 | Lower cretaceous | RAD MUDSTONE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 15 | 0 | 0 | 2 | 0 | 2 | 1 | 0 | 1 | 0 | 77 | 0 | 3 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
576.65 | 43-387-37-2,85 | 0 | 13 | 87 | Lower cretaceous | CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 8 | 0 | 0 | 1 | 0 | 2 | 2 | 0 | 2 | 0 | 87 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
578.20 | 43-387-37-3,90 | 5 | 20 | 75 | Lower cretaceous | RAD MUDSTONE | Dominat lithology; relative abundance | 5 | 0 | 0 | 2 | 12 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 1 | 0 | 74 | 0 | 5 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
579.55 | 43-387-37-4,75 | 5 | 15 | 80 | Lower cretaceous | RAD MUDSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 1 | 0 | 2 | 1 | 0 | 1 | 0 | 80 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
593.75 | 43-387-38-1,65 | 0 | 50 | 50 | Lower cretaceous | CHALK | Dominat lithology; relative abundance | 87 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 10 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
594.43 | 43-387-38-11,133 | 0 | 50 | 50 | Lower cretaceous | MARLY CHALK | Minor lithology; relative abundance | 64 | 0 | 5 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 30 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
623.00 | 43-387-39-11,140 | 0 | 0 | 0 | Lower cretaceous | CHALK | Dominat lithology; relative abundance | 81 | 0 | 3 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
624.07 | 43-387-39-2,97 | 3 | 67 | 30 | Lower cretaceous | CHALK | Dominat lithology; numerical abundance | 73 | 0 | 10 | 3 | 0 | 0 | 0 | 1 | 3 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
624.47 | 43-387-39-21,137 | 0 | 75 | 25 | Lower cretaceous | LIMESTONE | Dominat lithology; relative abundance | 89 | 0 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
632.25 | 43-387-40-11,115 | 10 | 65 | 25 | Lower cretaceous | LIMESTONE | Dominat lithology; relative abundance | 89 | 0 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
632.46 | 43-387-40-11,136 | 10 | 30 | 60 | Lower cretaceous | PYRITIC CHALK | Minor lithology; relative abundance | 40 | 2 | 15 | 0 | 5 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 22 | 0 | 15 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
633.30 | 43-387-40-2,70 | 5 | 20 | 75 | Lower cretaceous | CHALK OR LIMESTONE ? | Dominat lithology; numerical abundance | 80 | 1 | 6 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 10 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
641.21 | 43-387-41-1,61 | 1 | 33 | 66 | Lower cretaceous | MARLY NANNO CHALK | Dominat lithology; relative abundance | 7 | 0 | 30 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 1 | 0 | 53 | 0 | 0 | 7 | 0 | 2 | 2 | 0 | 0 | 76 |
641.73 | 43-387-41-11,113 | 0 | 60 | 40 | Lower cretaceous | CHALK | Dominat lithology; relative abundance | 86 | 1 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 10 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 |
642.20 | 43-387-41-CC,0 | 0 | 70 | 30 | Lower cretaceous | LIMESTONE | Dominat lithology; relative abundance | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 30 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 |
650.92 | 43-387-42-1,72 | 0 | 30 | 70 | Lower cretaceous | LIMESTONE | Dominat lithology; relative abundance | 94 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 6 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
669.30 | 43-387-43-CC,0 | 0 | 80 | 20 | Lower cretaceous | LIMESTONE | Dominat lithology; numerical abundance | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 |
679.92 | 43-387-44-11,122 | 0 | 65 | 35 | Lower cretaceous | LIMESTONE | Dominat lithology; relative abundance | 88 | 0 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 6 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 23 | 94 |
679.94 | 43-387-44-11,124 | 0 | 15 | 85 | Lower cretaceous | MARLY LIMESTONE | Dominat lithology; relative abundance | 59 | 0 | 2 | 2 | 3 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 32 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
699.00 | 43-387-45-11,130 | 0 | 30 | 70 | Lower cretaceous | MARLY LIMESTONE | Dominat lithology; numerical abundance | 45 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 12 | 0 | 0 | 0 | 2 | 0 | 37 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 97 |
727.20 | 43-387-46-11,120 | 0 | 0 | 0 | Lower cretaceous | SIDERITE LIMESTONE | Dominat lithology; numerical abundance | 65 | 0 | 6 | 2 | 0 | 0 | 0 | 1 | 15 | 0 | 0 | 0 | 2 | 0 | 12 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
727.20 | 43-387-46-11,120 | 5 | 50 | 45 | Lower cretaceous | SIDERITE RHOMBS | Minor lithology; relative 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 |
727.87 | 43-387-46-2,37 | 5 | 35 | 60 | Lower cretaceous | CALCAREOUS SILTY CLAYSTONE | Minor lithology; relative abundance | 25 | 0 | 3 | 2 | 0 | 0 | 0 | 17 | 1 | 0 | 0 | 0 | 2 | 0 | 49 | 0 | 5 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
728.01 | 43-387-46-2,51 | 0 | 50 | 50 | Lower cretaceous | LIMESTONE | Dominat lithology; relative abundance | 79 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
728.32 | 43-387-46-2,82 | 0 | 0 | 0 | Lower cretaceous | SIDERITE AND ALTERED MATERIAL | Dominat lithology; relative abundance | 25 | 0 | 12 | 0 | 0 | 0 | 0 | 1 | 21 | 0 | 2 | 0 | 2 | 0 | 20 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
728.32 | 43-387-46-2,82 | 5 | 55 | 40 | Lower cretaceous | SIDERITE LIMESTONE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 21 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
745.92 | 43-387-47-11,102 | 5 | 40 | 55 | Lower cretaceous | SIDERITE LIMESTONE | Dominat lithology; relative abundance | 65 | 0 | 15 | 2 | 0 | 0 | 0 | 0 | 15 | 0 | 2 | 0 | 2 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
764.59 | 43-387-48-1,89 | 5 | 40 | 55 | Lower cretaceous | CALCAREOUS SILTY CLAYSTONE | Minor lithology; relative abundance | 25 | 0 | 2 | 2 | 0 | 0 | 0 | 26 | 2 | 0 | 0 | 0 | 1 | 0 | 42 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
764.63 | 43-387-48-1,93 | 1 | 44 | 55 | Lower cretaceous | LIMESTONE | Dominat lithology; relative abundance | 89 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 1 | 0 | 0 | 0 | 2 | 0 | 6 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
783.68 | 43-387-49-11,128 | 0 | 0 | 0 | Lower cretaceous | INSOLUBLE IN 10% HYDROCHLORIC ACID RESIDUE OF THE BLACK MARLY LIMESTONE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 20 | 5 | 2 | 0 | 2 | 0 | 65 | 0 | 0 | 5 | 0 | 0 | 2 | 0 | 0 | 0 |
783.68 | 43-387-49-11,128 | 0 | 40 | 60 | Lower cretaceous | SIDERITE CALCAREOUS SILTY CLAYSTONE | Dominat lithology; relative abundance | 12 | 0 | 15 | 0 | 2 | 0 | 0 | 0 | 18 | 0 | 2 | 0 | 3 | 0 | 48 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 0 | 88 |
783.74 | 43-387-49-11,134 | 0 | 60 | 40 | Lower cretaceous | LIMESTONE | Dominat lithology; relative abundance | 83 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 0 | 0 | 2 | 0 | 7 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 98 |
783.87 | 43-387-49-11,147 | 0 | 71 | 29 | Lower cretaceous | LIMESTONE | Dominat lithology; numerical abundance | 82 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 7 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 94 |
784.62 | 43-387-49-2,72 | 3 | 35 | 60 | Lower cretaceous | SIDERITIC LIMESTONE (ROCK TYPE 4) | Dominat lithology; relative abundance | 48 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 15 | 2 | 0 | 0 | 0 | 0 | 26 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 |
784.63 | 43-387-49-2,73 | 5 | 29 | 66 | Lower cretaceous | SIDERITIC CALCAREOUS SILTY CLAYSTONE | Dominat lithology; relative abundance | 7 | 0 | 8 | 0 | 0 | 0 | 0 | 0 | 18 | 0 | 2 | 0 | 1 | 0 | 66 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 |
786.10 | 43-387-49-3,70 | 1 | 50 | 50 | Lower cretaceous | LIMESTONE (ROCK TYPE 2) | Dominat lithology; relative abundance | 83 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
787.02 | 43-387-49-4,12 | 5 | 40 | 55 | Lower cretaceous | SIDERITIC CALCAREOUS SILTY CLAYSTONE (COARSE BASE LAYER OF THE TYPE 3) | Minor lithology; relative abundance | 25 | 0 | 10 | 0 | 10 | 0 | 0 | 0 | 15 | 2 | 0 | 0 | 2 | 0 | 47 | 0 | 0 | 5 | 0 | 2 | 0 | 0 | 0 | 0 |
787.12 | 43-387-49-4,22 | 3 | 47 | 50 | Lower cretaceous | SIDERITIC CALCAREOUS SILTY CLAYSTONE (ROCK TYPE 3) | Dominat lithology; relative abundance | 35 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 2 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
789.80 | 43-387-49-51,140 | 0 | 50 | 50 | Lower cretaceous | LIMESTONE (ROCK TYPE 1) | Dominat lithology; relative abundance | 90 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |