Lewis, Brian T R; Robinson, Paul T (2005): Smear slide analysis of Hole 65-485A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230935
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
Zolotarev, Boris P; Stephen, Ralph A; Schmincke, Hans-Ulrich; Salisbury, Matthew H; Rangin, Claude; Morrison, M Ann; Kudo, A M; Hattner, J; Gutiérrez-Estrada, Mario; Flower, Martin F J; Duennebier, Frederick K; Day, Ron; Cambon, P; Blackinton, Grant; Benson, Richard N; Lewis, Brian T R; Robinson, P (1983): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, LXV, 752 pp, https://doi.org/10.2973/dsdp.proc.65.1983
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 22.748700 * Longitude: -107.903800
Date/Time Start: 1979-03-05T00:00:00 * Date/Time End: 1979-03-05T00:00:00
Minimum DEPTH, sediment/rock: 51.25 m * Maximum DEPTH, sediment/rock: 314.55 m
Event(s):
65-485A * Latitude: 22.748700 * Longitude: -107.903800 * Date/Time: 1979-03-05T00:00:00 * Elevation: -2981.0 m * Penetration: 331 m * Recovery: 136.1 m * Location: North Pacific/Gulf of California/SEDIMENT POND * Campaign: Leg65 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 38 cores; 271 m cored; 9.5 m drilled; 50.2 % recovery
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Sample code/label | Sample label | DSDP/ODP/IODP sample designation | |||
3 | Sand | Sand | % | Smear slide analysis | ||
4 | Silt | Silt | % | Smear slide analysis | ||
5 | Size fraction < 0.002 mm, clay | <2 µm | % | Smear slide analysis | ||
6 | Stratigraphy | Stratigraphy | Smear slide analysis | |||
7 | Lithology/composition/facies | Lithology | Smear slide analysis | |||
8 | Comment | Comment | Smear slide analysis | |||
9 | Carbonates | Carb | % | Smear slide analysis | ||
10 | Nannofossils | Nannos | % | Smear slide analysis | ||
11 | Foraminifera | Foram | % | Smear slide analysis | ||
12 | Radiolarians | Rad | % | Smear slide analysis | ||
13 | Diatoms | Diatoms | % | Smear slide analysis | ||
14 | Silicoflagellates | Silicoflag | % | Smear slide analysis | ||
15 | Spiculae | Spiculae | % | Smear slide analysis | ||
16 | Quartz | Qz | % | Smear slide analysis | ||
17 | Feldspar | Fsp | % | Smear slide analysis | ||
18 | Zeolite | Zeo | % | Smear slide analysis | ||
19 | Mica | Mica | % | Smear slide analysis | ||
20 | Clay minerals | Clay min | % | Smear slide analysis | ||
21 | Glauconite | Glt | % | Smear slide analysis | ||
22 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
23 | Heavy minerals | HM | % | Smear slide analysis | ||
24 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
25 | Palagonite | Palagonite | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1652 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 Diatoms [%] | 14 Silicoflag [%] | 15 Spiculae [%] | 16 Qz [%] | 17 Fsp [%] | 18 Zeo [%] | 19 Mica [%] | 20 Clay min [%] | 21 Glt [%] | 22 Py [%] | 23 HM [%] | 24 Volc glass [%] | 25 Palagonite [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
51.25 | 65-485A-1-1,75 | 4 | 37 | 59 | Quaternary | CALC NANNOS SANDY SILTY CLAY | Dominat lithology; relative abundance | 0 | 20 | 0 | 2 | 7 | 1 | 5 | 3 | 1 | 0 | 0 | 59 | 0 | 1 | 3 | 0 | 0 |
54.98 | 65-485A-1-31,148 | 7 | 23 | 70 | Quaternary | CALC NANNOS SILTY CLAY | Dominat lithology; relative abundance | 0 | 12 | 2 | 2 | 2 | 2 | 1 | 10 | 1 | 0 | 0 | 70 | 0 | 1 | 3 | 0 | 0 |
55.31 | 65-485A-1-4,31 | 7 | 21 | 72 | Quaternary | CALC NANNOS SILTY CLAY | Dominat lithology; relative abundance | 0 | 10 | 2 | 2 | 1 | 2 | 2 | 10 | 2 | 0 | 2 | 72 | 0 | 2 | 3 | 0 | 0 |
55.75 | 65-485A-1-4,75 | 5 | 9 | 86 | Quaternary | CLAY | Dominat lithology; relative abundance | 0 | 2 | 2 | 2 | 2 | 2 | 2 | 8 | 0 | 0 | 0 | 86 | 0 | 1 | 3 | 0 | 0 |
57.20 | 65-485A-1-5,70 | 1 | 20 | 79 | Quaternary | CALC NANNOS CLAY | Dominat lithology; relative abundance | 0 | 15 | 0 | 0 | 0 | 2 | 0 | 3 | 0 | 0 | 0 | 79 | 0 | 3 | 0 | 0 | 0 |
57.70 | 65-485A-1-51,120 | 1 | 50 | 49 | Quaternary | Dominat lithology; relative abundance | 3 | 20 | 0 | 2 | 0 | 0 | 2 | 20 | 3 | 0 | 0 | 49 | 0 | 2 | 2 | 0 | 0 | |
59.22 | 65-485A-1-61,122 | 15 | 55 | 30 | Quaternary | CALC NANNOS SANDY CLAYEY SILT | numerical abundance | 2 | 15 | 0 | 0 | 1 | 0 | 0 | 25 | 5 | 0 | 1 | 30 | 0 | 20 | 2 | 0 | 0 |
59.58 | 65-485A-1-7,8 | 2 | 33 | 65 | Quaternary | CALC NANNOS SILTY CLAY | Dominat lithology; numerical abundance | 0 | 10 | 0 | 0 | 1 | 0 | 0 | 15 | 2 | 0 | 0 | 65 | 0 | 5 | 2 | 0 | 0 |
59.70 | 65-485A-1-7,20 | 0 | 38 | 62 | Quaternary | CALC NANNOS SILTY CLAY | Dominat lithology; numerical abundance | 0 | 12 | 0 | 0 | 1 | 0 | 0 | 20 | 3 | 0 | 0 | 62 | 0 | 1 | 1 | 0 | 0 |
59.90 | 65-485A-1-7,40 | 0 | 46 | 54 | Quaternary | CALC NANNOS SILTY CLAY | relative abundance | 0 | 16 | 1 | 0 | 1 | 0 | 0 | 20 | 3 | 0 | 2 | 54 | 0 | 2 | 3 | 0 | 0 |
60.75 | 65-485A-2-1,75 | 0 | 45 | 55 | Upper quaternary | CALC NANNOS SILTY CLAY | Dominat lithology; relative abundance | 0 | 20 | 2 | 0 | 1 | 0 | 0 | 20 | 1 | 0 | 0 | 55 | 0 | 1 | 2 | 0 | 0 |
64.17 | 65-485A-2-31,117 | 1 | 44 | 55 | Upper quaternary | CALC NANNOS SILTY CLAY | Dominat lithology; relative abundance | 2 | 20 | 1 | 0 | 1 | 0 | 1 | 20 | 2 | 0 | 0 | 55 | 0 | 0 | 1 | 0 | 0 |
64.87 | 65-485A-2-4,37 | 20 | 27 | 53 | Upper quaternary | CALC NANNOS SANDY SILTY CLAY | numerical abundance | 5 | 10 | 1 | 1 | 1 | 0 | 1 | 20 | 2 | 0 | 0 | 53 | 0 | 4 | 2 | 0 | 0 |
65.15 | 65-485A-2-4,65 | 20 | 24 | 56 | Upper quaternary | CALC NANNOS SANDY SILTY CLAY | Dominat lithology; relative abundance | 2 | 10 | 2 | 2 | 1 | 1 | 0 | 22 | 2 | 0 | 0 | 56 | 0 | 3 | 1 | 0 | 0 |
65.37 | 65-485A-2-4,87 | 0 | 42 | 58 | Upper quaternary | CALC NANNOS SILTY CLAY | Dominat lithology; numerical abundance | 0 | 25 | 0 | 0 | 1 | 0 | 0 | 10 | 1 | 0 | 1 | 58 | 0 | 1 | 3 | 0 | 0 |
65.55 | 65-485A-2-41,105 | 2 | 26 | 72 | Upper quaternary | CALC NANNOS SILTY CLAY | relative abundance | 0 | 16 | 2 | 2 | 3 | 2 | 1 | 5 | 0 | 0 | 0 | 72 | 0 | 1 | 2 | 0 | 0 |
70.27 | 65-485A-3-1,77 | 1 | 22 | 77 | Upper quaternary | CALC NANNOS CLAY | Dominat lithology; relative abundance | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | 0 | 77 | 0 | 1 | 2 | 0 | 0 |
70.90 | 65-485A-3-11,140 | 10 | 27 | 63 | Upper quaternary | CALC NANNOS SANDY SILTY CLAY | Minor lithology; relative abundance | 2 | 10 | 0 | 2 | 2 | 0 | 2 | 20 | 2 | 0 | 1 | 63 | 0 | 1 | 1 | 0 | 0 |
72.20 | 65-485A-3-21,120 | 0 | 42 | 58 | Upper quaternary | CALC NANNOS SILTY CLAY | Dominat lithology; relative abundance | 0 | 15 | 0 | 1 | 1 | 1 | 2 | 20 | 2 | 0 | 0 | 58 | 0 | 1 | 1 | 0 | 0 |
73.06 | 65-485A-3-3,56 | 5 | 51 | 44 | Upper quaternary | SANDY CLAYEY SILT | Dominat lithology; relative abundance | 0 | 10 | 5 | 2 | 1 | 0 | 1 | 20 | 2 | 0 | 0 | 44 | 0 | 15 | 0 | 2 | 0 |
92.25 | 65-485A-5-3,75 | 0 | 25 | 75 | Quaternary | CALC NANNOS CLAY | Dominat lithology; relative abundance | 0 | 15 | 2 | 0 | 1 | 0 | 0 | 7 | 0 | 0 | 0 | 75 | 0 | 1 | 2 | 0 | 0 |
93.52 | 65-485A-5-4,52 | 3 | 32 | 65 | Quaternary | CALC NANNOS SANDY SILTY CLAY | Dominat lithology; relative abundance | 0 | 20 | 0 | 0 | 1 | 0 | 2 | 10 | 2 | 0 | 0 | 65 | 0 | 1 | 1 | 0 | 0 |
98.75 | 65-485A-6-1,75 | 0 | 30 | 70 | Quaternary | CALC NANNOS SILTY CLAY | Dominat lithology; relative abundance | 0 | 15 | 0 | 0 | 2 | 0 | 0 | 10 | 1 | 0 | 0 | 70 | 0 | 1 | 3 | 0 | 0 |
101.84 | 65-485A-6-3,84 | 0 | 25 | 75 | Quaternary | CALC NANNOS SILTY CLAY | relative abundance | 0 | 15 | 2 | 0 | 2 | 0 | 0 | 7 | 1 | 0 | 0 | 75 | 0 | 1 | 1 | 0 | 0 |
101.86 | 65-485A-6-3,86 | 6 | 39 | 55 | Quaternary | CALC NANNOS SANDY SILTY CLAY | Dominat lithology; relative abundance | 15 | 15 | 1 | 0 | 1 | 0 | 0 | 10 | 1 | 0 | 2 | 55 | 0 | 1 | 2 | 0 | 0 |
108.23 | 65-485A-7-1,73 | 5 | 22 | 73 | Quaternary | CALC NANNOS SANDY SILTY CLAY | relative abundance | 10 | 10 | 0 | 0 | 0 | 2 | 2 | 6 | 2 | 0 | 0 | 73 | 0 | 2 | 1 | 0 | 0 |
109.12 | 65-485A-7-2,12 | 5 | 16 | 89 | Quaternary | CALC NANNOS CLAY | Dominat lithology; relative abundance | 8 | 8 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 0 | 0 | 75 | 0 | 2 | 1 | 0 | 0 |
119.25 | 65-485A-8-2,75 | 0 | 33 | 67 | Quaternary | CALC NANNOS SILTY CLAY | Dominat lithology; relative abundance | 8 | 15 | 2 | 1 | 1 | 0 | 0 | 5 | 0 | 0 | 0 | 67 | 0 | 1 | 2 | 0 | 0 |
128.75 | 65-485A-9-2,75 | 60 | 35 | 5 | Quaternary | Dominat lithology; relative abundance | 25 | 3 | 1 | 0 | 0 | 0 | 0 | 65 | 2 | 0 | 2 | 5 | 0 | 1 | 1 | 2 | 0 | |
136.75 | 65-485A-10-1,75 | 10 | 37 | 53 | Quaternary | SANDY SILTY CLAY | Dominat lithology; relative abundance | 2 | 25 | 2 | 0 | 2 | 0 | 0 | 15 | 1 | 0 | 2 | 53 | 0 | 5 | 2 | 1 | 0 |
137.31 | 65-485A-10-11,131 | 15 | 61 | 24 | Quaternary | SANDY CLAYEY SILT | Dominat lithology; relative abundance | 15 | 20 | 1 | 0 | 0 | 0 | 0 | 30 | 5 | 0 | 2 | 24 | 2 | 5 | 1 | 0 | 2 |
138.25 | 65-485A-10-2,75 | 0 | 99 | 1 | Quaternary | CALC NANNO SILT | Dominat lithology; relative abundance | 10 | 50 | 0 | 0 | 3 | 0 | 0 | 20 | 2 | 0 | 2 | 1 | 2 | 10 | 2 | 1 | 0 |
146.25 | 65-485A-11-1,75 | 2 | 60 | 38 | Quaternary | CLAYEY SILT | Dominat lithology; relative abundance | 10 | 7 | 2 | 0 | 2 | 0 | 0 | 33 | 5 | 0 | 2 | 38 | 0 | 1 | 2 | 2 | 0 |
147.75 | 65-485A-11-2,75 | 2 | 65 | 33 | Quaternary | CLAYEY SILT | Dominat lithology; relative abundance | 20 | 20 | 1 | 0 | 2 | 0 | 0 | 20 | 3 | 0 | 2 | 33 | 0 | 2 | 1 | 2 | 0 |
148.85 | 65-485A-11-3,35 | 60 | 35 | 5 | Quaternary | SILTY SAND | Dominat lithology; numerical abundance | 10 | 5 | 5 | 0 | 0 | 0 | 0 | 40 | 15 | 0 | 5 | 5 | 0 | 5 | 5 | 0 | 0 |
184.45 | 65-485A-18-1,95 | 25 | 31 | 44 | Quaternary | SANDY SILTY CLAY | relative abundance | 3 | 7 | 1 | 0 | 1 | 0 | 0 | 35 | 5 | 0 | 2 | 44 | 0 | 2 | 2 | 0 | 0 |
189.52 | 65-485A-19-2,2 | 25 | 14 | 61 | Quaternary | SILTY SANDY CLAY | relative abundance | 5 | 5 | 1 | 0 | 1 | 0 | 2 | 20 | 2 | 0 | 0 | 61 | 0 | 2 | 3 | 0 | 0 |
190.23 | 65-485A-19-2,73 | 20 | 21 | 59 | Quaternary | numerical abundance | 0 | 7 | 0 | 1 | 1 | 0 | 0 | 10 | 2 | 0 | 3 | 59 | 0 | 15 | 2 | 0 | 0 | |
190.92 | 65-485A-19-21,142 | 0 | 83 | 17 | Quaternary | CALC NANNOS CLAYEY SILT | Dominat lithology; relative abundance | 0 | 50 | 0 | 0 | 1 | 0 | 0 | 30 | 2 | 0 | 0 | 17 | 0 | 1 | 1 | 0 | 0 |
193.02 | 65-485A-20-1,52 | 0 | 60 | 40 | Quaternary | CALC NANNOS CLAYEY SILT | numerical abundance | 0 | 30 | 0 | 0 | 3 | 0 | 0 | 25 | 0 | 0 | 0 | 40 | 0 | 1 | 1 | 0 | 0 |
194.61 | 65-485A-20-CC,24 | 0 | 61 | 39 | Quaternary | CALC NANNOS CLAYED SILT | numerical abundance | 30 | 10 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 39 | 0 | 0 | 1 | 0 | 0 |
201.60 | 65-485A-22-1,10 | 1 | 45 | 54 | Quaternary | CALC NANNOS SILTY CLAY | relative abundance | 2 | 30 | 2 | 0 | 1 | 0 | 0 | 12 | 1 | 0 | 2 | 54 | 0 | 1 | 1 | 0 | 0 |
204.00 | 65-485A-22-21,100 | 0 | 62 | 38 | Quaternary | CALC NANNOS CLAYED SILT | numerical abundance | 5 | 30 | 1 | 0 | 1 | 0 | 0 | 20 | 2 | 0 | 0 | 38 | 0 | 2 | 1 | 0 | 0 |
204.68 | 65-485A-22-3,18 | 0 | 57 | 43 | Quaternary | CALC NANNOS CLAYED SILT | Dominat lithology; relative abundance | 0 | 40 | 0 | 0 | 3 | 2 | 0 | 10 | 0 | 0 | 0 | 43 | 0 | 1 | 3 | 0 | 0 |
205.85 | 65-485A-22-31,135 | 40 | 21 | 39 | Quaternary | CALC NANNOS SILTY CLAYED SAND | numerical abundance | 0 | 15 | 2 | 0 | 3 | 0 | 0 | 30 | 5 | 0 | 0 | 39 | 0 | 3 | 3 | 0 | 0 |
206.20 | 65-485A-22-4,20 | 2 | 60 | 38 | Quaternary | CALC NANNOS SANDY CLAYED SILT | relative abundance | 2 | 40 | 1 | 0 | 2 | 0 | 0 | 15 | 1 | 0 | 2 | 38 | 0 | 2 | 1 | 0 | 0 |
207.22 | 65-485A-22-41,122 | 0 | 68 | 32 | Quaternary | CLAYED SILT | relative abundance | 2 | 50 | 0 | 0 | 1 | 0 | 2 | 10 | 2 | 0 | 2 | 32 | 0 | 5 | 2 | 0 | 0 |
209.80 | 65-485A-22-6,80 | 1 | 67 | 32 | Quaternary | CALC NANNOS CLAYED SILT | relative abundance | 2 | 50 | 0 | 0 | 1 | 0 | 0 | 12 | 2 | 0 | 2 | 32 | 0 | 4 | 1 | 0 | 0 |
211.55 | 65-485A-23-1,5 | 5 | 64 | 31 | Quaternary | CARBONATED SANDY CLAYEY SILT | Dominat lithology; relative abundance | 50 | 3 | 0 | 2 | 1 | 0 | 0 | 10 | 3 | 0 | 0 | 31 | 0 | 3 | 0 | 0 | 0 |
211.85 | 65-485A-23-1,35 | 10 | 30 | 60 | Quaternary | SANDY SILTY CLAY | Dominat lithology; relative abundance | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 22 | 1 | 0 | 2 | 60 | 0 | 5 | 2 | 0 | 0 |
226.40 | 65-485A-26-1,40 | 0 | 62 | 38 | Quaternary | CALC NANNO CLAY | Dominat lithology; relative abundance | 1 | 50 | 0 | 0 | 2 | 0 | 0 | 5 | 2 | 0 | 2 | 38 | 0 | 7 | 2 | 0 | 0 |
226.75 | 65-485A-26-1,75 | 0 | 51 | 49 | Quaternary | CALC NANNO CLAY | Dominat lithology; relative abundance | 1 | 40 | 2 | 0 | 2 | 0 | 0 | 7 | 1 | 0 | 0 | 49 | 0 | 3 | 2 | 2 | 0 |
227.64 | 65-485A-26-2,14 | 0 | 46 | 54 | Quaternary | CALC NANNO CLAY | Dominat lithology; relative abundance | 1 | 40 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | 0 | 54 | 0 | 1 | 1 | 1 | 0 |
230.70 | 65-485A-27-1,20 | 0 | 32 | 68 | Quaternary | SILTY CLAY | Dominat lithology; relative abundance | 1 | 20 | 2 | 0 | 0 | 0 | 0 | 10 | 1 | 0 | 0 | 68 | 0 | 0 | 2 | 2 | 0 |
231.76 | 65-485A-27-11,126 | 0 | 40 | 60 | Quaternary | CALC NANNOS CLAY | Dominat lithology; relative abundance | 1 | 30 | 0 | 0 | 2 | 0 | 0 | 5 | 2 | 0 | 0 | 60 | 0 | 5 | 1 | 2 | 0 |
236.25 | 65-485A-28-11,125 | 0 | 41 | 59 | Quaternary | PYRITIC CLAY | Dominat lithology; relative abundance | 1 | 20 | 0 | 0 | 2 | 0 | 0 | 5 | 2 | 0 | 0 | 59 | 0 | 15 | 1 | 2 | 0 |
270.49 | 65-485A-33-2,99 | 3 | 10 | 87 | Quaternary | SANDY SILTY CLAY | Minor lithology; relative abundance | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 5 | 0 | 87 | 0 | 2 | 2 | 0 | 0 |
277.14 | 65-485A-34-1,14 | 0 | 11 | 89 | Quaternary | CLAY | Dominat lithology; numerical abundance | 1 | 1 | 0 | 0 | 1 | 0 | 0 | 5 | 0 | 0 | 0 | 89 | 0 | 2 | 1 | 0 | 0 |
277.55 | 65-485A-34-1,55 | 4 | 11 | 85 | Quaternary | SANDY SILTY CLAY | Dominat lithology; relative abundance | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 7 | 0 | 3 | 0 | 85 | 0 | 2 | 2 | 0 | 0 |
295.37 | 65-485A-36-1,37 | 0 | 32 | 68 | Quaternary | SILTY CLAY | Dominat lithology; relative abundance | 1 | 5 | 1 | 0 | 2 | 0 | 0 | 5 | 5 | 0 | 0 | 78 | 0 | 5 | 1 | 1 | 0 |
295.66 | 65-485A-36-1,66 | 0 | 14 | 86 | Quaternary | Dominat lithology; relative abundance | 0 | 10 | 0 | 0 | 2 | 0 | 0 | 3 | 2 | 5 | 0 | 86 | 0 | 1 | 1 | 2 | 0 | |
297.32 | 65-485A-36-2,82 | 0 | 26 | 74 | Quaternary | CALC NANNO MUD | Dominat lithology; relative abundance | 1 | 20 | 2 | 0 | 2 | 0 | 0 | 1 | 2 | 0 | 2 | 74 | 0 | 5 | 2 | 2 | 0 |
298.64 | 65-485A-36-3,64 | 0 | 0 | 0 | Quaternary | CALC NANNOS CLAY | Dominat lithology; relative abundance | 34 | 34 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 25 | 2 | 0 | 0 |
298.71 | 65-485A-36-3,71 | 0 | 100 | 0 | Quaternary | CARBONATE COATING BASALT | Dominat lithology; relative abundance | 85 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 |
304.75 | 65-485A-37-1,75 | 0 | 21 | 79 | Quaternary | CLAY | Dominat lithology; relative abundance | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 3 | 1 | 5 | 2 | 79 | 0 | 2 | 1 | 2 | 0 |
313.10 | 65-485A-38-1,10 | 0 | 27 | 73 | Quaternary | CALC NANNOS SILTY CLAY | Dominat lithology; relative abundance | 1 | 10 | 0 | 0 | 0 | 0 | 0 | 10 | 2 | 0 | 0 | 73 | 0 | 3 | 1 | 2 | 0 |
313.85 | 65-485A-38-1,85 | 0 | 20 | 80 | Quaternary | FINE GRAINED SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 1 | 0 | 2 | 80 | 0 | 5 | 2 | 2 | 0 |
314.46 | 65-485A-38-11,146 | 0 | 27 | 73 | Quaternary | SILTY CLAY | Dominat lithology; numerical abundance | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 12 | 2 | 0 | 0 | 73 | 0 | 10 | 1 | 0 | 0 |
314.55 | 65-485A-38-2,5 | 0 | 22 | 78 | Quaternary | SILTY CLAY | Dominat lithology; relative abundance | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 1 | 2 | 0 | 78 | 0 | 10 | 1 | 2 | 0 |