Heath, G Ross; Burckle, Lloyd H (2005): Smear slide analysis of Hole 86-576B [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.231135
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
Wright, Audrey; Schultheiss, P; Morley, Joseph J; Lenôtre, Nicole; Monechi, Simonetta; Krissek, Lawrence A; Koizumi, Itaru; Janecek, Thomas R; Jacobi, Robert D; Horai, Ki-Iti; Bleil, Ulrich; D'Agostino, Anthony E; Heath, G Ross; Burckle, Lloyd H (1985): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, LXXXVI, 804 pp, https://doi.org/10.2973/dsdp.proc.86.1985
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 32.356200 * Longitude: 164.275300
Date/Time Start: 1982-05-16T00:00:00 * Date/Time End: 1982-05-16T00:00:00
Minimum DEPTH, sediment/rock: 0.90 m * Maximum DEPTH, sediment/rock: 72.61 m
Event(s):
86-576B * Latitude: 32.356200 * Longitude: 164.275300 * Date/Time: 1982-05-16T00:00:00 * Elevation: -6217.0 m * Penetration: 74.8 m * Recovery: 74.1 m * Location: North Pacific * Campaign: Leg86 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 9 cores; 74.8 m cored; 0 m drilled; 99 % 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 | Lithology/composition/facies | Lithology | Smear slide analysis | |||
7 | Comment | Comment | Smear slide analysis | |||
8 | Carbonates | Carb | % | Smear slide analysis | ||
9 | Nannofossils | Nannos | % | Smear slide analysis | ||
10 | Foraminifera | Foram | % | Smear slide analysis | ||
11 | Radiolarians | Rad | % | Smear slide analysis | ||
12 | Diatoms | Diatoms | % | Smear slide analysis | ||
13 | Silicoflagellates | Silicoflag | % | Smear slide analysis | ||
14 | Spiculae | Spiculae | % | Smear slide analysis | ||
15 | Quartz | Qz | % | Smear slide analysis | ||
16 | Feldspar | Fsp | % | Smear slide analysis | ||
17 | Zeolite | Zeo | % | Smear slide analysis | ||
18 | Mica | Mica | % | Smear slide analysis | ||
19 | Clay minerals | Clay min | % | Smear slide analysis | ||
20 | Glauconite | Glt | % | Smear slide analysis | ||
21 | Opaque minerals | Opaque | % | Smear slide analysis | ||
22 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
23 | Iron | Fe | % | Smear slide analysis | ||
24 | Limonite | Lm | % | Smear slide analysis | ||
25 | Heavy minerals | HM | % | Smear slide analysis | ||
26 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
27 | Palagonite | Palagonite | % | Smear slide analysis | ||
28 | Terrigenous | Terr | % | Smear slide analysis | terrigeneous detritus | |
29 | Micronodules | Micronod | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1680 data points
Data
1 Depth sed [m] | 2 Sample label | 3 Sand [%] | 4 Silt [%] | 5 <2 µm [%] | 6 Lithology | 7 Comment | 8 Carb [%] | 9 Nannos [%] | 10 Foram [%] | 11 Rad [%] | 12 Diatoms [%] | 13 Silicoflag [%] | 14 Spiculae [%] | 15 Qz [%] | 16 Fsp [%] | 17 Zeo [%] | 18 Mica [%] | 19 Clay min [%] | 20 Glt [%] | 21 Opaque [%] | 22 Py [%] | 23 Fe [%] | 24 Lm [%] | 25 HM [%] | 26 Volc glass [%] | 27 Palagonite [%] | 28 Terr [%] | 29 Micronod [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.90 | 86-576B-1-1,90 | 5 | 15 | 80 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 5 | 2 | 2 | 2 | 8 | 2 | 0 | 0 | 79 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 1 |
1.98 | 86-576B-1-2,48 | 5 | 20 | 75 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 5 | 2 | 2 | 2 | 10 | 2 | 0 | 0 | 75 | 0 | 0 | 0 | 1 | 0 | 0 | 4 | 0 | 0 | 2 |
5.25 | 86-576B-1-4,75 | 3 | 12 | 85 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 2 | 2 | 2 | 2 | 12 | 2 | 0 | 0 | 81 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 2 |
7.76 | 86-576B-1-6,26 | 1 | 10 | 89 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 1 | 2 | 0 | 2 | 12 | 2 | 0 | 0 | 84 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 2 |
8.23 | 86-576B-2-1,3 | 2 | 15 | 20 | BROWN CLAY (PELAGIC) | numerical abundance | 0 | 0 | 0 | 5 | 0 | 0 | 1 | 7 | 2 | 0 | 0 | 83 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 100 | 0 |
8.23 | 86-576B-2-1,3 | 20 | 60 | 83 | VOLCANIC ASH | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 7 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 88 | 0 | 0 | 0 |
9.40 | 86-576B-2-11,120 | 5 | 20 | 75 | PELAGIC CLAY | numerical abundance | 0 | 0 | 0 | 10 | 1 | 0 | 1 | 10 | 1 | 0 | 0 | 75 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 |
10.40 | 86-576B-2-2,70 | 1 | 15 | 84 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 5 | 2 | 0 | 2 | 15 | 5 | 2 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 |
12.16 | 86-576B-2-3,96 | 2 | 10 | 88 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 10 | 2 | 2 | 0 | 88 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 |
12.21 | 86-576B-2-31,101 | 2 | 12 | 86 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 2 | 0 | 2 | 2 | 10 | 2 | 0 | 0 | 86 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 |
13.00 | 86-576B-2-4,30 | 1 | 12 | 87 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 2 | 0 | 0 | 87 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 2 |
13.10 | 86-576B-2-4,40 | 15 | 65 | 20 | VOLCANIC ASH | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 90 | 0 | 0 | 0 |
13.70 | 86-576B-2-41,100 | 0 | 0 | 0 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 7 | 1 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 2 |
14.60 | 86-576B-2-5,40 | 20 | 60 | 20 | VOLCANIC ASH | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 1 | 1 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 90 | 0 | 0 | 0 |
15.10 | 86-576B-2-5,90 | 2 | 12 | 88 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 1 | 0 | 0 | 85 | 0 | 0 | 0 | 1 | 0 | 0 | 3 | 0 | 0 | 2 |
15.65 | 86-576B-2-51,145 | 1 | 10 | 89 | M QTZ 7,FEL 1,MICA 1,CLAY 86,VOLC.GLAS 3, HEMA 1,MICRONOD 1 | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
16.00 | 86-576B-2-6,30 | 0 | 6 | 94 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | 0 | 95 | 0 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 2 |
16.80 | 86-576B-2-61,110 | 0 | 10 | 90 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 7 | 2 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 2 |
18.20 | 86-576B-3-1,50 | 1 | 9 | 90 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 7 | 2 | 0 | 0 | 90 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 1 |
21.20 | 86-576B-3-3,50 | 2 | 15 | 83 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 7 | 2 | 83 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 1 |
21.94 | 86-576B-3-31,124 | 1 | 7 | 92 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | 2 | 91 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 1 |
22.60 | 86-576B-3-4,40 | 0 | 10 | 90 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 7 | 2 | 0 | 2 | 89 | 0 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 1 |
24.50 | 86-576B-3-5,80 | 0 | 8 | 92 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 7 | 2 | 0 | 0 | 89 | 0 | 0 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 2 |
25.90 | 86-576B-3-6,70 | 0 | 7 | 93 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 2 | 0 | 1 | 90 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 1 |
27.00 | 86-576B-3-7,30 | 0 | 12 | 88 | M QTZ 5,CLAY 85,OP 3,VOLC.GLAS TR,MICRONOD TR, ZEOL 7 | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
29.10 | 86-576B-4-2,40 | 0 | 10 | 90 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 5 | 2 | 88 | 0 | 0 | 0 | 4 | 0 | 0 | 1 | 0 | 0 | 2 |
32.10 | 86-576B-4-4,40 | 0 | 8 | 92 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 2 | 5 | 2 | 84 | 0 | 0 | 0 | 3 | 0 | 0 | 2 | 0 | 0 | 2 |
33.48 | 86-576B-4-5,28 | 0 | 9 | 91 | M QTZ 1,FEL TR,MICA 1,CLAY 91,VOLC.GLAS TR, HEMA 2,MICRONOD TR,ZEOL 5 | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
34.85 | 86-576B-4-6,15 | 1 | 2 | 97 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 2 | 2 | 97 | 0 | 0 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 |
36.40 | 86-576B-4-7,20 | 0 | 4 | 96 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 2 | 0 | 2 | 96 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 2 |
38.70 | 86-576B-5-2,50 | 1 | 6 | 93 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 2 | 2 | 0 | 2 | 92 | 0 | 4 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 1 |
40.70 | 86-576B-5-31,100 | 0 | 7 | 93 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 2 | 2 | 96 | 0 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 1 |
43.50 | 86-576B-5-5,80 | 0 | 5 | 95 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 2 | 2 | 95 | 0 | 0 | 0 | 3 | 0 | 0 | 1 | 0 | 0 | 1 |
45.36 | 86-576B-5-61,116 | 2 | 2 | 96 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 0 | 96 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 1 |
48.20 | 86-576B-6-2,50 | 2 | 4 | 94 | PELAGIC CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 94 | 0 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 2 |
50.20 | 86-576B-6-31,100 | 1 | 2 | 97 | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 97 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 2 | 0 | 2 |
51.00 | 86-576B-6-4,30 | 2 | 10 | 88 | PELAGIC CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 3 | 0 | 0 | 78 | 0 | 10 | 0 | 0 | 0 | 0 | 4 | 0 | 100 | 0 |
51.70 | 86-576B-6-41,100 | 0 | 5 | 95 | PELAGIC CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 3 | 0 | 0 | 85 | 0 | 0 | 0 | 3 | 2 | 0 | 2 | 0 | 100 | 0 |
51.80 | 86-576B-6-41,110 | 0 | 10 | 90 | PELAGIC CLAY | relative abundance | 0 | 2 | 2 | 2 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 89 | 0 | 3 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
51.95 | 86-576B-6-41,125 | 1 | 14 | 85 | NANNO OOZE | relative abundance | 0 | 81 | 2 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | 0 | 10 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 19 | 0 |
52.40 | 86-576B-6-5,20 | 0 | 50 | 50 | NANNOFOSSIL OOZE | relative abundance | 5 | 0 | 70 | 0 | 0 | 0 | 0 | 5 | 0 | 2 | 0 | 15 | 1 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 |
53.25 | 86-576B-6-51,105 | 0 | 10 | 90 | PELAGIC CLAY | numerical abundance | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 2 | 0 | 83 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
53.90 | 86-576B-6-6,20 | 0 | 40 | 60 | NANNOFOSSIL OOZE | numerical abundance | 15 | 50 | 0 | 0 | 0 | 0 | 0 | 7 | 0 | 3 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 |
54.80 | 86-576B-6-61,110 | 1 | 9 | 90 | NANNO OOZE | relative abundance | 0 | 85 | 2 | 0 | 0 | 0 | 0 | 3 | 1 | 0 | 0 | 10 | 0 | 2 | 0 | 0 | 0 | 0 | 1 | 0 | 15 | 0 |
55.44 | 86-576B-6-CC,32 | 1 | 19 | 80 | NANNO OOZE | numerical abundance | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 5 | 0 |
55.74 | 86-576B-7-1,4 | 3 | 12 | 85 | NANNO OOZE | numerical abundance | 0 | 73 | 3 | 0 | 0 | 0 | 0 | 7 | 2 | 0 | 0 | 10 | 0 | 3 | 0 | 0 | 0 | 0 | 2 | 0 | 24 | 0 |
56.70 | 86-576B-7-11,100 | 0 | 10 | 90 | NANNO OOZE | numerical abundance | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 5 | 3 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 20 | 0 |
57.95 | 86-576B-7-2,75 | 1 | 19 | 80 | NANNO OOZE | relative abundance | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 7 | 3 | 0 | 0 | 10 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 20 | 0 |
59.20 | 86-576B-7-3,50 | 0 | 40 | 60 | NANNOFOSSIL OOZE | numerical abundance | 1 | 70 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 20 | 0 | 0 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | 1 |
59.85 | 86-576B-7-31,115 | 5 | 15 | 80 | NANNO OOZE | numerical abundance | 0 | 75 | 5 | 0 | 0 | 0 | 0 | 4 | 1 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 20 | 0 |
59.90 | 86-576B-7-31,120 | 6 | 20 | 74 | NANNO OOZE | numerical abundance | 0 | 67 | 5 | 0 | 0 | 0 | 0 | 7 | 2 | 0 | 0 | 15 | 0 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 28 | 0 |
60.00 | 86-576B-7-31,130 | 3 | 17 | 80 | NANNO OOZE | numerical abundance | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 5 | 3 | 0 | 0 | 7 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 20 | 0 |
60.95 | 86-576B-7-4,75 | 0 | 50 | 50 | NANNO OOZE | relative abundance | 0 | 65 | 2 | 0 | 0 | 0 | 0 | 20 | 0 | 1 | 0 | 10 | 1 | 0 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
63.55 | 86-576B-7-6,35 | 0 | 15 | 85 | PELAGIC CLAY | relative abundance | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 82 | 0 | 10 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
64.45 | 86-576B-7-61,125 | 0 | 60 | 40 | NANNOFOSSIL OOZE | relative abundance | 0 | 75 | 2 | 0 | 0 | 0 | 0 | 10 | 0 | 1 | 0 | 10 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
66.50 | 86-576B-8-11,130 | 7 | 23 | 70 | NANNO OOZE | relative abundance | 0 | 61 | 7 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | 0 | 25 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 32 | 0 |
67.40 | 86-576B-8-2,70 | 4 | 15 | 81 | NANNO OOZE | numerical abundance | 0 | 80 | 3 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 0 | 4 | 0 | 3 | 0 | 0 | 0 | 0 | 2 | 0 | 17 | 0 |
71.00 | 86-576B-8-41,130 | 0 | 60 | 40 | NANNOFOSSIL OOZE | numerical abundance | 0 | 80 | 1 | 0 | 0 | 0 | 0 | 5 | 0 | 1 | 0 | 5 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 1 |
71.55 | 86-576B-8-5,35 | 5 | 25 | 70 | NANNO OOZE | numerical abundance | 0 | 77 | 3 | 0 | 0 | 0 | 0 | 7 | 3 | 0 | 0 | 8 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 20 | 0 |
72.61 | 86-576B-8-51,141 | 0 | 25 | 75 | CALCAREOUS CLAY | numerical abundance | 10 | 20 | 1 | 0 | 0 | 0 | 0 | 10 | 0 | 2 | 0 | 50 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 |