Yeats, Robert S; Haq, Bilal U (2005): Smear slide analysis of Hole 63-473 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230909
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
Wolfart, R; Shibata, Tsugio; Poore, Richard Z; Pisciotto, Kenneth A; Verma, Surendra P; Niem, Alan; Leinen, Margaret W; Grechin, V I; Douglas, A G; Denham, C R; Crouch, James; Bukry, David; Barron, John A; Yeats, Robert S; Haq, Bilal U (1981): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, LXIII, 967 pp, https://doi.org/10.2973/dsdp.proc.63.1981
Further details:
Processed smear slide data base - background and methods. hdl:10013/epic.32353.d001
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 20.965300 * Longitude: -107.063500
Date/Time Start: 1978-11-22T00:00:00 * Date/Time End: 1978-11-22T00:00:00
Minimum DEPTH, sediment/rock: 0.13 m * Maximum DEPTH, sediment/rock: 248.08 m
Event(s):
63-473 * Latitude: 20.965300 * Longitude: -107.063500 * Date/Time: 1978-11-22T00:00:00 * Elevation: -3249.0 m * Penetration: 287.5 m * Recovery: 141.6 m * Location: North Pacific/Gulf of California/CONT RISE * Campaign: Leg63 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 34 cores; 287.5 m cored; 0 m drilled; 49.3 % recovery
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Sample code/label | Sample label | DSDP/ODP/IODP sample designation | |||
3 | Sand | Sand | % | Smear slide analysis | ||
4 | Silt | Silt | % | Smear slide analysis | ||
5 | Size fraction < 0.002 mm, clay | <2 µm | % | Smear slide analysis | ||
6 | Stratigraphy | Stratigraphy | Smear slide analysis | |||
7 | Lithology/composition/facies | Lithology | Smear slide analysis | |||
8 | Comment | Comment | Smear slide analysis | |||
9 | Carbonates | Carb | % | Smear slide analysis | ||
10 | Nannofossils | Nannos | % | Smear slide analysis | ||
11 | Foraminifera | Foram | % | Smear slide analysis | ||
12 | Opal, biogenic silica | bSiO2 | % | Smear slide analysis | ||
13 | Radiolarians | Rad | % | Smear slide analysis | ||
14 | Diatoms | Diatoms | % | Smear slide analysis | ||
15 | Silicoflagellates | Silicoflag | % | Smear slide analysis | ||
16 | Spiculae | Spiculae | % | Smear slide analysis | ||
17 | Quartz | Qz | % | Smear slide analysis | ||
18 | Feldspar | Fsp | % | Smear slide analysis | ||
19 | Zeolite | Zeo | % | Smear slide analysis | ||
20 | Mica | Mica | % | Smear slide analysis | ||
21 | Biotite | Bt | % | 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 | Heavy minerals | HM | % | Smear slide analysis | ||
28 | Zircon | Zrn | % | Smear slide analysis | ||
29 | Apatite | Ap | % | Smear slide analysis | ||
30 | Hornblende | Hbl | % | Smear slide analysis | ||
31 | Amphibole | Amp | % | Smear slide analysis | ||
32 | Pyroxene | Pyrox | % | Smear slide analysis | ||
33 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
34 | Rock fragments | Rock fragm | % | Smear slide analysis | ||
35 | Terrigenous | Terr | % | Smear slide analysis | terrigeneous detritus |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1900 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 bSiO2 [%] | 13 Rad [%] | 14 Diatoms [%] | 15 Silicoflag [%] | 16 Spiculae [%] | 17 Qz [%] | 18 Fsp [%] | 19 Zeo [%] | 20 Mica [%] | 21 Bt [%] | 22 Clay min [%] | 23 Glt [%] | 24 Opaque [%] | 25 Py [%] | 26 Fe [%] | 27 HM [%] | 28 Zrn [%] | 29 Ap [%] | 30 Hbl [%] | 31 Amp [%] | 32 Pyrox [%] | 33 Volc glass [%] | 34 Rock fragm [%] | 35 Terr [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.13 | 63-473-1-CC,13 | 0 | 15 | 85 | Quaternary | SILTY CLAY | Dominat lithology; relative abundance | 2 | 2 | 2 | 0 | 1 | 4 | 2 | 0 | 5 | 2 | 0 | 2 | 0 | 80 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
0.70 | 63-473-2-1,20 | 0 | 17 | 83 | Quaternary | SILTY CLAY | Dominat lithology; relative abundance | 2 | 1 | 2 | 0 | 1 | 3 | 2 | 2 | 5 | 3 | 0 | 2 | 0 | 80 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
4.01 | 63-473-2-3,51 | 0 | 18 | 82 | Quaternary | SILTY CLAY | Minor lithology; relative abundance | 2 | 2 | 2 | 0 | 2 | 3 | 2 | 2 | 5 | 2 | 0 | 2 | 2 | 80 | 2 | 0 | 5 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
5.88 | 63-473-2-4,88 | 0 | 0 | 0 | Quaternary | VITRIC ASH | Dominat 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 | 1 | 0 | 0 |
10.30 | 63-473-3-1,30 | 0 | 17 | 83 | Quaternary | CLAY | Dominat lithology; relative abundance | 2 | 3 | 1 | 0 | 2 | 5 | 2 | 2 | 3 | 2 | 0 | 2 | 2 | 80 | 2 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
12.93 | 63-473-3-21,143 | 0 | 0 | 0 | Quaternary | VITRIC ASH | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 97 | 0 | 0 |
20.53 | 63-473-4-11,103 | 0 | 15 | 85 | Quaternary | NANNOFOSSIL CLAY | Dominat lithology; relative abundance | 2 | 15 | 2 | 0 | 1 | 2 | 2 | 2 | 4 | 2 | 0 | 0 | 0 | 20 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
29.80 | 63-473-5-1,80 | 0 | 13 | 87 | Quaternary | NANNOFOSSIL CLAY | Dominat lithology; relative abundance | 2 | 15 | 5 | 0 | 2 | 1 | 2 | 2 | 3 | 2 | 0 | 2 | 0 | 72 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
31.70 | 63-473-5-21,120 | 0 | 100 | 0 | Quaternary | VITRIC ASH | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 12 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 0 |
38.90 | 63-473-6-1,40 | 0 | 13 | 87 | Quaternary | NANNOFOSSIL CLAY | Dominat lithology; relative abundance | 0 | 12 | 2 | 0 | 2 | 2 | 2 | 2 | 3 | 2 | 0 | 2 | 0 | 75 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
39.00 | 63-473-6-1,50 | 0 | 15 | 85 | Quaternary | NANNOFOSSIL CLAY | relative abundance | 0 | 16 | 0 | 0 | 2 | 2 | 2 | 2 | 6 | 2 | 0 | 2 | 0 | 72 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 80 |
50.35 | 63-473-7-2,85 | 0 | 5 | 95 | Quaternary | CLAY | Dominat lithology; relative abundance | 2 | 6 | 2 | 0 | 2 | 2 | 0 | 1 | 6 | 1 | 0 | 1 | 0 | 80 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
58.00 | 63-473-8-1,50 | 0 | 9 | 91 | Quaternary | CLAY | relative abundance | 2 | 7 | 1 | 0 | 2 | 0 | 0 | 2 | 4 | 2 | 0 | 2 | 0 | 84 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 90 |
68.21 | 63-473-9-11,121 | 0 | 8 | 92 | Quaternary | CLAY | relative abundance | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 5 | 2 | 0 | 2 | 0 | 92 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 97 |
78.50 | 63-473-10-2,50 | 0 | 10 | 90 | Quaternary | CLAY | relative abundance | 3 | 2 | 2 | 0 | 2 | 0 | 0 | 2 | 3 | 2 | 0 | 2 | 0 | 90 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 93 |
87.06 | 63-473-11-11,106 | 0 | 6 | 94 | Upper pliocene | CLAY | Dominat lithology; relative abundance | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 4 | 1 | 0 | 1 | 0 | 91 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
96.00 | 63-473-12-1,50 | 0 | 7 | 93 | Upper pliocene | relative abundance | 0 | 1 | 1 | 0 | 0 | 0 | 2 | 2 | 3 | 2 | 0 | 2 | 0 | 92 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 95 | |
106.20 | 63-473-13-11,120 | 10 | 48 | 42 | Upper pliocene | SANDY SILT | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 7 | 0 | 1 | 0 | 0 | 2 | 3 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 0 |
115.10 | 63-473-14-1,60 | 0 | 15 | 85 | Upper pliocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 7 | 5 | 0 | 2 | 0 | 85 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 0 |
115.90 | 63-473-14-11,140 | 0 | 20 | 80 | Upper pliocene | CALCAREOUS CLAY | Minor lithology; relative abundance | 15 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 2 | 0 | 2 | 0 | 80 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
117.03 | 63-473-14-21,103 | 0 | 10 | 90 | Upper pliocene | ALTERED TUFF (?) | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 3 | 1 | 0 | 1 | 90 | 0 | 0 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
125.45 | 63-473-15-11,145 | 0 | 40 | 57 | Upper pliocene | CALCAREOUS CLAY | Minor lithology; relative abundance | 40 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 0 | 2 | 0 | 57 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
127.50 | 63-473-15-3,50 | 0 | 6 | 94 | Upper pliocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 2 | 2 | 2 | 0 | 94 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
129.04 | 63-473-15-4,54 | 0 | 15 | 85 | Upper pliocene | ALTERED TUFFACEOUS (?) SILTY CLAYSTONE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 5 | 1 | 2 | 1 | 85 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 |
134.77 | 63-473-16-11,127 | 0 | 40 | 60 | Lower pliocene | ALTERED TUFF | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 0 | 0 |
136.84 | 63-473-16-3,34 | 0 | 0 | 0 | Lower pliocene | CLAYEY VITRIC TUFF | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 3 | 0 | 0 | 0 | 43 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 |
136.91 | 63-473-16-3,41 | 0 | 0 | 0 | Lower pliocene | VITRIC TUFF | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 0 |
138.27 | 63-473-16-4,27 | 0 | 9 | 81 | Lower pliocene | CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 2 | 1 | 0 | 0 | 81 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
141.99 | 63-473-16-CC,0 | 0 | 25 | 75 | Lower pliocene | DIATOMACEOUS CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 2 | 10 | 5 | 1 | 4 | 2 | 0 | 0 | 0 | 75 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
145.77 | 63-473-17-21,127 | 0 | 40 | 60 | Lower pliocene | DIATOMACEOUS CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 1 | 25 | 6 | 1 | 3 | 2 | 0 | 2 | 0 | 60 | 2 | 0 | 2 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
147.82 | 63-473-17-4,32 | 0 | 90 | 10 | Lower pliocene | PYRITIZED DIATOMACEOUS OOZE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 2 | 50 | 5 | 3 | 3 | 2 | 0 | 2 | 0 | 10 | 0 | 0 | 25 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
149.06 | 63-473-17-5,6 | 60 | 23 | 17 | Lower pliocene | DIATOMACEOUS SILTY SANDSTONE | Minor lithology; relative abundance | 5 | 0 | 0 | 0 | 1 | 15 | 1 | 1 | 25 | 10 | 0 | 2 | 0 | 17 | 2 | 0 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 10 | 10 | 0 |
153.10 | 63-473-18-1,60 | 0 | 50 | 50 | Lower pliocene | DIATOMACEOUS CLAYSTONE | Dominat lithology; relative abundance | 1 | 0 | 0 | 0 | 2 | 35 | 5 | 1 | 3 | 2 | 0 | 2 | 0 | 50 | 2 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
153.98 | 63-473-18-11,148 | 0 | 100 | 0 | Lower pliocene | VITRIC TUFF (ASH) | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 0 |
162.73 | 63-473-19-1,73 | 0 | 5 | 95 | Lower pliocene | LIGHT MOTTLE/CALCAREOUS CLAYSTONE | Minor lithology; relative abundance | 25 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 1 | 0 | 2 | 0 | 55 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
162.80 | 63-473-19-1,80 | 0 | 30 | 70 | Lower pliocene | TUFFACEOUS CLAYSTONE | Dominat lithology; relative abundance | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 2 | 2 | 2 | 0 | 65 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 0 |
167.90 | 63-473-19-41,140 | 0 | 15 | 85 | Lower pliocene | CLAYSTONE | Dominat lithology; relative abundance | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 2 | 3 | 2 | 2 | 2 | 0 | 85 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
174.10 | 63-473-20-21,110 | 0 | 15 | 85 | Lower pliocene | NANNO CLAYSTONE | Dominat lithology; relative abundance | 2 | 10 | 0 | 0 | 2 | 5 | 3 | 2 | 3 | 2 | 2 | 2 | 2 | 75 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
179.23 | 63-473-20-6,23 | 0 | 70 | 30 | Lower pliocene | SILICEOUS CHALK | Minor lithology; relative abundance | 35 | 25 | 0 | 0 | 2 | 15 | 5 | 2 | 1 | 1 | 0 | 0 | 0 | 14 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
181.50 | 63-473-21-1,50 | 1 | 29 | 70 | Lower pliocene | SILICEOUS SILTY CLAYSTONE | relative abundance | 1 | 2 | 2 | 0 | 4 | 8 | 1 | 1 | 12 | 3 | 0 | 2 | 0 | 67 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 82 |
182.27 | 63-473-21-11,127 | 2 | 40 | 58 | Lower pliocene | SILTY CLAYSTONE | relative abundance | 0 | 2 | 1 | 0 | 1 | 4 | 2 | 1 | 18 | 8 | 0 | 2 | 0 | 56 | 0 | 0 | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 85 |
184.75 | 63-473-21-3,75 | 0 | 67 | 33 | Upper miocene | SILICEOUS NANNO CHALK | Minor lithology; relative abundance | 45 | 20 | 0 | 0 | 5 | 16 | 2 | 2 | 1 | 2 | 0 | 0 | 0 | 13 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 14 |
186.00 | 63-473-21-4,50 | 0 | 6 | 94 | Upper miocene | CLAYSTONE | Dominat lithology; relative abundance | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 1 | 0 | 2 | 0 | 90 | 2 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
191.00 | 63-473-23-1,50 | 0 | 15 | 85 | Upper miocene | CLAYSTONE | relative abundance | 0 | 2 | 0 | 0 | 2 | 1 | 1 | 0 | 9 | 2 | 0 | 0 | 0 | 83 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 94 |
202.00 | 63-473-24-2,50 | 0 | 30 | 70 | Upper miocene | SILTY CLAYSTONE | relative abundance | 0 | 1 | 0 | 0 | 1 | 2 | 2 | 2 | 23 | 3 | 0 | 2 | 0 | 69 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 95 |
203.15 | 63-473-24-3,15 | 0 | 15 | 85 | Upper miocene | SILTY CLAYSTONE | Dominat lithology; relative abundance | 0 | 2 | 2 | 2 | 0 | 0 | 0 | 0 | 15 | 2 | 0 | 2 | 0 | 81 | 2 | 0 | 1 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 |
203.57 | 63-473-24-CC,8 | 0 | 25 | 75 | Upper miocene | SILTY CLAYSTONE | Dominat lithology; relative abundance | 0 | 2 | 2 | 0 | 2 | 2 | 0 | 2 | 20 | 2 | 0 | 1 | 0 | 72 | 2 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
211.72 | 63-473-25-CC,0 | 0 | 40 | 60 | Upper miocene | SILTY CLAYSTONE | numerical abundance | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 25 | 6 | 0 | 1 | 0 | 60 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 98 |
219.51 | 63-473-26-1,51 | 60 | 24 | 16 | Upper miocene | SILTY QUARTOSE SANDS | Minor lithology; relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 10 | 0 | 5 | 0 | 16 | 2 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 5 | 0 |
219.66 | 63-473-26-1,66 | 0 | 60 | 40 | Upper miocene | CLAYEY SILTSTONE | relative abundance | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 50 | 6 | 0 | 2 | 0 | 40 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 100 |
219.73 | 63-473-26-1,73 | 35 | 56 | 9 | Upper miocene | SANDY SILTSTONE | relative abundance | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 64 | 12 | 0 | 5 | 0 | 9 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 4 | 95 |
220.84 | 63-473-26-2,34 | 0 | 6 | 94 | Upper miocene | ALTERED TUFFACEOUS CLAY | Minor lithology; relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 2 | 0 | 69 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 0 |
229.28 | 63-473-27-1,78 | 0 | 40 | 60 | Upper miocene | SILTY CLAYSTONE | relative abundance | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 3 | 0 | 2 | 0 | 60 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 93 |
247.95 | 63-473-29-1,45 | 0 | 20 | 80 | SILTY CLAYSTONE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 7 | 5 | 0 | 0 | 0 | 80 | 0 | 0 | 7 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | |
248.05 | 63-473-29-1,55 | 70 | 30 | 0 | SILTY SANDSTONE | Minor lithology; relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 10 | 1 | 0 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 2 | 2 | 60 | 0 | |
248.08 | 63-473-29-1,58 | 80 | 20 | 0 | SILTY SANDSTONE | Minor lithology; relative abundance | 8 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 25 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 5 | 0 | 0 | 10 | 0 |