Hussong, Donald M; Uyeda, Seiya (2005): Smear slide analysis of Hole 60-453 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230879
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
Sharaskin, Anatoly; Packham, G H; Natland, James H; Nakamura, K; Meijer, Arend; Kling, Stanley; Horai, Ki-Iti; Francis, T J G; Ellis, C Howard; Bleil, Ulrich; Blanchet, R; Hussong, Donald M; Uyeda, Seiya (1982): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, LX, 929 pp, https://doi.org/10.2973/dsdp.proc.60.1982
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 17.907000 * Longitude: 143.682500
Date/Time Start: 1978-03-28T00:00:00 * Date/Time End: 1978-03-28T00:00:00
Minimum DEPTH, sediment/rock: 0.30 m * Maximum DEPTH, sediment/rock: 446.37 m
Event(s):
60-453 * Latitude: 17.907000 * Longitude: 143.682500 * Date/Time: 1978-03-28T00:00:00 * Elevation: -4693.0 m * Penetration: 605 m * Recovery: 235.1 m * Location: North Pacific/SEDIMENT POND * Campaign: Leg60 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 63 cores; 595.5 m cored; 9.5 m drilled; 39.5 % 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 | 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 | Clay minerals | Clay min | % | Smear slide analysis | ||
22 | Opaque minerals | Opaque | % | Smear slide analysis | ||
23 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
24 | Iron | Fe | % | Smear slide analysis | ||
25 | Heavy minerals | HM | % | Smear slide analysis | ||
26 | Pyroxene | Pyrox | % | Smear slide analysis | ||
27 | Olivine | Ol | % | Smear slide analysis | ||
28 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
29 | Rock fragments | Rock fragm | % | Smear slide analysis | ||
30 | Micronodules | Micronod | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
6632 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 Silicoflag [%] | 16 Spiculae [%] | 17 Qz [%] | 18 Fsp [%] | 19 Zeo [%] | 20 Mica [%] | 21 Clay min [%] | 22 Opaque [%] | 23 Py [%] | 24 Fe [%] | 25 HM [%] | 26 Pyrox [%] | 27 Ol [%] | 28 Volc glass [%] | 29 Rock fragm [%] | 30 Micronod [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.30 | 60-453-1-1,30 | 0 | 40 | 60 | Upper pleistocene | SILICEOUS OOZE | relative abundance | 0 | 0 | 0 | 1 | 10 | 20 | 0 | 3 | 2 | 5 | 0 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 0 |
1.84 | 60-453-1-2,34 | 0 | 60 | 40 | Upper pleistocene | DIATOMACEOUS OOZE | relative abundance | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 1 | 9 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 0 | 0 |
2.45 | 60-453-1-2,95 | 0 | 30 | 70 | Upper pleistocene | SILICEOUS MUD | relative abundance | 0 | 0 | 0 | 0 | 10 | 8 | 0 | 1 | 2 | 10 | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
2.50 | 60-453-1-21,100 | 0 | 60 | 40 | Upper pleistocene | DIATOMACEOUS OOZE | numerical abundance | 0 | 0 | 0 | 0 | 15 | 35 | 0 | 5 | 2 | 5 | 0 | 0 | 35 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 1 |
6.50 | 60-453-1-5,50 | 0 | 40 | 60 | Upper pleistocene | SILICEOUS PELAGIC MUD | numerical abundance | 0 | 0 | 0 | 0 | 5 | 10 | 0 | 2 | 3 | 5 | 0 | 0 | 58 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 15 |
7.35 | 60-453-1-51,135 | 1 | 19 | 80 | Upper pleistocene | VITRIC MUD WITH DIATOMS | relative abundance | 0 | 0 | 2 | 0 | 2 | 8 | 0 | 2 | 1 | 5 | 0 | 0 | 68 | 0 | 0 | 0 | 2 | 0 | 0 | 10 | 0 | 2 |
8.00 | 60-453-1-6,50 | 1 | 39 | 60 | Upper pleistocene | VITRIC MUD | relative abundance | 0 | 0 | 2 | 0 | 5 | 2 | 0 | 2 | 3 | 5 | 0 | 0 | 58 | 0 | 0 | 0 | 2 | 0 | 0 | 15 | 5 | 5 |
9.30 | 60-453-1-CC,0 | 0 | 30 | 70 | Upper pleistocene | SILICEOUS OOZE | relative abundance | 0 | 0 | 0 | 0 | 20 | 10 | 0 | 1 | 0 | 10 | 0 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
9.60 | 60-453-2-1,60 | 0 | 40 | 60 | Upper pleistocene | SILICEOUS OOZE | relative abundance | 0 | 0 | 0 | 0 | 10 | 20 | 0 | 2 | 0 | 8 | 0 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
10.00 | 60-453-2-11,100 | 0 | 20 | 80 | Upper pleistocene | SILICEOUS PELAGIC MUD | relative abundance | 0 | 0 | 0 | 0 | 6 | 4 | 0 | 0 | 1 | 10 | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 |
11.40 | 60-453-2-2,90 | 0 | 20 | 80 | Upper pleistocene | PELAGIC SILICEOUS MUD | relative abundance | 0 | 0 | 0 | 0 | 10 | 5 | 0 | 2 | 0 | 8 | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 |
12.30 | 60-453-2-3,30 | 1 | 39 | 60 | Upper pleistocene | SILICEOUS MUD | relative abundance | 0 | 0 | 0 | 0 | 15 | 5 | 0 | 1 | 1 | 5 | 0 | 0 | 60 | 0 | 0 | 1 | 0 | 0 | 0 | 5 | 5 | 3 |
13.80 | 60-453-2-4,30 | 0 | 40 | 60 | Upper pleistocene | SILICEOUS MUD - VITRIC LITHIC MUD | relative abundance | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 1 | 3 | 10 | 0 | 1 | 48 | 0 | 0 | 0 | 2 | 0 | 0 | 20 | 10 | 0 |
15.08 | 60-453-2-CC,0 | 0 | 30 | 70 | Upper pleistocene | MUD VITRIC CRYTAL MUD | relative abundance | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 1 | 0 | 10 | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 |
19.20 | 60-453-3-1,70 | 0 | 40 | 60 | Lower pleistocene | MUD CRYSTAL-LITHIC MUD | relative abundance | 0 | 0 | 0 | 0 | 5 | 2 | 1 | 0 | 5 | 20 | 0 | 0 | 53 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 10 | 0 |
19.90 | 60-453-3-11,140 | 2 | 28 | 70 | Lower pleistocene | MUD SILICEOUS LITHIC MUD | relative abundance | 0 | 0 | 1 | 1 | 5 | 0 | 1 | 1 | 2 | 10 | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 13 | 0 |
20.60 | 60-453-3-2,60 | 0 | 35 | 65 | Lower pleistocene | MUD W/ROCK FRAGS(VOLC) XALS LITHIC MUD | relative abundance | 0 | 0 | 0 | 0 | 3 | 1 | 0 | 0 | 2 | 15 | 0 | 0 | 65 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 |
20.90 | 60-453-3-2,90 | 10 | 30 | 60 | Lower pleistocene | MUD W/ROCK FRAGS(VOLC) XALS VITRIC MUD | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 10 | 0 | 0 | 57 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 20 | 0 |
21.78 | 60-453-3-CC,0 | 1 | 20 | 79 | Lower pleistocene | MUD | numerical abundance | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 1 | 0 | 6 | 0 | 0 | 79 | 0 | 0 | 0 | 1 | 0 | 0 | 3 | 6 | 2 |
28.65 | 60-453-4-1,65 | 0 | 5 | 95 | Lower pleistocene | ZEOLITIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 7 | 3 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
30.15 | 60-453-4-2,65 | 0 | 8 | 92 | Lower pleistocene | CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 5 | 1 | 0 | 92 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 1 |
31.65 | 60-453-4-3,65 | 0 | 0 | 100 | Lower pleistocene | MUD | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 10 | 1 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 |
33.15 | 60-453-4-4,65 | 0 | 15 | 85 | Lower pleistocene | MUD | relative abundance | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 85 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 5 | 1 |
34.65 | 60-453-4-5,65 | 0 | 5 | 95 | Lower pleistocene | ZEOLITIC PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 |
36.15 | 60-453-4-6,65 | 0 | 0 | 100 | Lower pleistocene | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 1 | 0 | 97 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 |
38.25 | 60-453-5-1,75 | 0 | 10 | 90 | Lower pleistocene | PELAGIC MUD | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 87 | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 3 |
39.50 | 60-453-5-2,50 | 0 | 5 | 95 | Lower pleistocene | PELAGIC MUD | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 2 | 0 | 87 | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 1 | 0 |
47.07 | 60-453-6-1,7 | 10 | 40 | 50 | Lower pleistocene | MUD LITHIC-CRYSTAL MUD | relative abundance | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 15 | 5 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 15 | 15 |
48.00 | 60-453-6-11,100 | 0 | 10 | 90 | Lower pleistocene | MUD | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 10 |
56.60 | 60-453-7-CC,0 | 1 | 9 | 90 | Lower pleistocene | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 90 | 0 | 0 | 2 | 2 | 0 | 0 | 2 | 2 | 3 |
66.85 | 60-453-8-1,85 | 2 | 8 | 90 | Lower pleistocene | ZEOLITIC PELAGIC MUD | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 3 | 0 | 85 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 7 |
68.20 | 60-453-8-2,70 | 0 | 10 | 90 | Lower pleistocene | PELAGIC CLAY | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 3 |
69.48 | 60-453-8-3,48 | 0 | 40 | 60 | Lower pleistocene | SILTY MUD - VITRIC MUD | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 1 | 0 | 60 | 0 | 0 | 0 | 0 | 1 | 0 | 30 | 0 | 0 |
70.20 | 60-453-8-31,120 | 0 | 7 | 93 | Lower pleistocene | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 5 | 0 | 0 | 91 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 2 |
70.95 | 60-453-8-4,45 | 0 | 40 | 60 | Lower pleistocene | SILTY VITRIC ASH | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 1 |
71.20 | 60-453-8-4,70 | 0 | 5 | 95 | Lower pleistocene | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 90 | 0 | 0 | 0 | 2 | 0 | 0 | 5 | 0 | 2 |
71.67 | 60-453-8-41,117 | 5 | 30 | 65 | Lower pleistocene | LITHIC-VITRIC CRYSTAL MUD | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 65 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 10 | 0 |
71.85 | 60-453-8-41,135 | 2 | 15 | 83 | Lower pleistocene | CRYSTAL VITRIC MUD | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 84 | 0 | 0 | 0 | 1 | 0 | 0 | 8 | 0 | 2 |
72.10 | 60-453-8-CC,0 | 0 | 20 | 80 | Lower pleistocene | MUD RICH VOLC.GLAS VITRIC MUD | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 0 | 72 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 5 | 0 |
75.66 | 60-453-9-1,16 | 0 | 5 | 95 | Lower pleistocene | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 |
75.69 | 60-453-9-1,19 | 0 | 20 | 80 | Lower pleistocene | LITHIC MUD | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 15 | 1 |
75.80 | 60-453-9-1,30 | 0 | 10 | 90 | Lower pleistocene | VITRIC MUD | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 1 | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 1 | 0 |
86.60 | 60-453-10-2,10 | 0 | 8 | 92 | Lower pleistocene | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 1 |
86.72 | 60-453-10-2,22 | 0 | 20 | 80 | Lower pleistocene | VITRIC MUD | relative abundance | 0 | 0 | 0 | 0 | 1 | 5 | 0 | 0 | 0 | 5 | 0 | 0 | 70 | 0 | 0 | 0 | 1 | 0 | 0 | 20 | 0 | 1 |
87.00 | 60-453-10-2,50 | 0 | 5 | 95 | Lower pleistocene | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 93 | 0 | 0 | 2 | 2 | 0 | 0 | 2 | 0 | 1 |
88.40 | 60-453-10-3,40 | 0 | 2 | 98 | Lower pleistocene | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 98 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
88.67 | 60-453-10-3,67 | 0 | 90 | 10 | Lower pleistocene | SILTY VITRIC ASH | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 10 | 0 | 0 | 0 | 1 | 0 | 0 | 84 | 0 | 0 |
88.90 | 60-453-10-CC,0 | 0 | 8 | 92 | Lower pleistocene | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 92 | 0 | 0 | 0 | 1 | 0 | 0 | 5 | 0 | 0 |
94.60 | 60-453-11-1,10 | 0 | 20 | 80 | Lower pleistocene | VITRIC MUDSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 80 | 0 | 0 | 1 | 0 | 0 | 0 | 15 | 1 | 0 |
94.67 | 60-453-11-1,17 | 0 | 10 | 90 | Lower pleistocene | PELAGIC CLAY (SILTY) | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
95.25 | 60-453-11-1,75 | 0 | 3 | 97 | Lower pleistocene | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 95 | 0 | 0 | 2 | 0 | 0 | 0 | 1 | 0 | 1 |
96.33 | 60-453-11-2,33 | 0 | 10 | 90 | Lower pleistocene | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 90 | 0 | 0 | 1 | 0 | 0 | 0 | 5 | 1 | 0 |
96.68 | 60-453-11-2,68 | 2 | 40 | 60 | Lower pleistocene | VITRIC MUD | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 58 | 0 | 0 | 0 | 1 | 0 | 0 | 37 | 1 | 0 |
98.25 | 60-453-11-3,75 | 0 | 30 | 70 | Lower pleistocene | SILTY MUD - CRYSTAL MUD | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
99.50 | 60-453-11-4,50 | 0 | 20 | 80 | Lower pleistocene | CRYSTAL MUD | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 80 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 1 |
100.73 | 60-453-11-5,23 | 0 | 30 | 70 | Lower pleistocene | CRYSTAL MUDSTONE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 70 | 0 | 0 | 0 | 1 | 0 | 0 | 3 | 0 | 2 |
105.12 | 60-453-12-11,112 | 0 | 20 | 80 | Lower pleistocene | CRYSTAL MUD | relative abundance | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 1 | 0 | 80 | 0 | 0 | 0 | 1 | 0 | 0 | 5 | 0 | 1 |
112.03 | 60-453-12-6,53 | 0 | 55 | 45 | Lower pleistocene | SILICEOUS OOZE - RADIOLARIAN OOZE | numerical abundance | 0 | 0 | 0 | 0 | 50 | 5 | 0 | 5 | 0 | 5 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 |
112.30 | 60-453-12-6,80 | 0 | 80 | 20 | Lower pleistocene | SILTY VITRIC ASH | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 20 | 0 | 0 | 0 | 1 | 0 | 0 | 75 | 0 | 0 |
114.27 | 60-453-13-1,77 | 0 | 35 | 65 | Upper pliocene | MUD WITH VOLC. GLASS, VITRIC XTALS MUD | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 65 | 0 | 0 | 0 | 1 | 0 | 0 | 20 | 0 | 0 |
114.37 | 60-453-13-1,87 | 50 | 45 | 5 | Upper pliocene | VOLCANIC SAND - SANDY VITRIC ASH | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 20 | 0 | 0 | 10 | 0 | 0 | 30 | 0 | 0 |
114.70 | 60-453-13-11,120 | 70 | 20 | 10 | Upper pliocene | SANDY SIZE MICRONOD LAYER | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 75 |
114.90 | 60-453-13-CC,0 | 0 | 5 | 95 | Upper pliocene | PELAGIC CLAY | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 2 | 90 | 0 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 1 |
123.20 | 60-453-14-1,20 | 2 | 8 | 90 | Upper pliocene | NANNOFOSSIL MUDSTONE | relative abundance | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 1 | 1 | 8 | 0 | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 0 |
123.24 | 60-453-14-1,24 | 1 | 20 | 80 | Upper pliocene | MUD | relative abundance | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 80 | 0 | 0 | 0 | 2 | 0 | 0 | 7 | 0 | 10 |
123.65 | 60-453-14-1,65 | 0 | 10 | 90 | Upper pliocene | MUDSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 1 |
124.21 | 60-453-14-11,121 | 0 | 10 | 90 | Upper pliocene | CLAYEY MUDSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | 89 | 0 | 0 | 2 | 2 | 0 | 0 | 3 | 0 | 1 |
124.60 | 60-453-14-2,10 | 0 | 5 | 95 | Upper pliocene | CLAYSTONE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 |
124.95 | 60-453-14-2,45 | 0 | 10 | 90 | Upper pliocene | MUDSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 10 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
125.93 | 60-453-14-CC,0 | 0 | 15 | 85 | Upper pliocene | MUDSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 85 | 0 | 0 | 0 | 1 | 0 | 0 | 1 | 0 | 10 |
132.80 | 60-453-15-1,30 | 0 | 5 | 95 | Upper pliocene | CLAYSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 |
133.90 | 60-453-15-11,140 | 0 | 1 | 99 | Upper pliocene | CLAYSTONE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
135.13 | 60-453-15-21,113 | 0 | 5 | 95 | Upper pliocene | PELAGIC CLAYSTONE | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 |
135.83 | 60-453-15-3,33 | 0 | 5 | 95 | Upper pliocene | PELAGIC CLAYSTONE | numerical abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 90 | 0 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 5 |
135.90 | 60-453-15-3,40 | 2 | 23 | 75 | Upper pliocene | VITRIC CRYSTAL MUD | relative abundance | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 65 | 0 | 0 | 0 | 3 | 0 | 0 | 12 | 0 | 5 |
135.97 | 60-453-15-3,47 | 0 | 20 | 80 | Upper pliocene | MUDSTONE | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 12 | 1 | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 8 |
136.28 | 60-453-15-3,78 | 0 | 15 | 85 | Upper pliocene | VITRIC MUDSTONE | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 82 | 0 | 0 | 0 | 2 | 0 | 0 | 10 | 0 | 5 |
136.40 | 60-453-15-CC,0 | 0 | 10 | 90 | Upper pliocene | PELAGIC CLAYSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 90 | 0 | 0 | 0 | 1 | 0 | 0 | 1 | 0 | 10 |
151.67 | 60-453-17-1,17 | 0 | 25 | 75 | Upper pliocene | MUD WITH ABUNDANT MICRONODULES | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 75 | 0 | 0 | 1 | 1 | 0 | 0 | 5 | 0 | 15 |
152.20 | 60-453-17-CC,0 | 1 | 39 | 60 | Upper pliocene | VITRIC MUD | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 60 | 0 | 0 | 0 | 1 | 0 | 0 | 15 | 0 | 20 |
162.04 | 60-453-18-11,104 | 0 | 30 | 70 | CALCAREOUS DOLOMITIC MUD | numerical abundance | 0 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
162.60 | 60-453-18-2,10 | 0 | 40 | 60 | CALCAREOUS (DOLOMITIC) MUD | numerical abundance | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
162.78 | 60-453-18-2,28 | 0 | 40 | 60 | CALCAREOUS PELAGIC MUD OR SEDIMENT | relative abundance | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 50 | 0 | 0 | 1 | 2 | 0 | 0 | 2 | 0 | 0 | |
163.84 | 60-453-18-21,134 | 1 | 60 | 40 | VITRIC MUD | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 50 | 0 | 0 | 0 | 1 | 0 | 0 | 20 | 0 | 20 | |
164.42 | 60-453-18-3,42 | 0 | 2 | 98 | PELAGIC CLAYSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 0 | 98 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
168.52 | 60-453-18-6,2 | 0 | 30 | 70 | MUDSTONE RICH IN MICRONODULES | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 5 | 0 | 64 | 0 | 0 | 0 | 1 | 0 | 0 | 5 | 0 | 25 | |
168.56 | 60-453-18-6,6 | 3 | 60 | 37 | VITRIC MUDSTONE RICH IN ZEOLITE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 25 | 0 | 30 | 0 | 0 | 0 | 1 | 0 | 0 | 30 | 0 | 5 | |
169.20 | 60-453-18-6,70 | 0 | 22 | 78 | MUD RICH IN MICRONODULES | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 78 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 15 | |
170.05 | 60-453-18-7,5 | 0 | 20 | 80 | VITRIC MUD WITH CARBONATES | relative abundance | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 80 | 0 | 0 | 0 | 1 | 0 | 0 | 15 | 0 | 0 | |
170.62 | 60-453-18-CC,15 | 0 | 30 | 70 | Lower pliocene | VITRIC MUDSTONE | numerical abundance | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 |
171.00 | 60-453-19-1,50 | 0 | 40 | 60 | Lower pliocene | MUD RICH IN VOLC. GLASS - VITRIC MUD | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 |
181.73 | 60-453-20-2,23 | 0 | 60 | 40 | Lower pliocene | CHALK (SILTY SIZE) | relative abundance | 70 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
182.20 | 60-453-20-2,70 | 0 | 30 | 75 | Lower pliocene | MUD RICH IN MICRONODULES | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 |
183.79 | 60-453-20-3,79 | 0 | 15 | 85 | Lower pliocene | ZEOLITIC MUDSTONE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 15 | 0 | 73 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 2 |
190.52 | 60-453-21-11,102 | 0 | 20 | 80 | Lower pliocene | MICRONODULES RICH MUDSTONE | relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 5 | 0 | 20 | 0 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 70 |
190.61 | 60-453-21-11,111 | 0 | 55 | 45 | Lower pliocene | MUD RICH IN MICRONOD - VITRIC MUDSTONE | relative abundance | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 55 | 0 | 0 | 1 | 0 | 0 | 0 | 10 | 0 | 35 |
190.97 | 60-453-21-11,147 | 0 | 5 | 95 | Lower pliocene | PELAGIC CLAYSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 3 | 1 | 0 | 95 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 |
191.09 | 60-453-21-2,9 | 0 | 60 | 40 | Lower pliocene | SILTY-VITRIC TUFF - VOLC GLASS MUD | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 2 |
191.40 | 60-453-21-2,40 | 0 | 30 | 70 | Lower pliocene | MUD RICH IN VOLC. GLASS - VITRIC MUDST | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 0 |
191.60 | 60-453-21-CC,0 | 5 | 30 | 65 | Lower pliocene | VITRIC MUDSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 60 | 0 | 0 | 0 | 2 | 0 | 0 | 30 | 0 | 2 |
199.10 | 60-453-22-1,10 | 0 | 40 | 60 | Lower pliocene | CRYSTAL-VITRIC MUD | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 1 | 0 |
199.33 | 60-453-22-1,33 | 0 | 2 | 98 | Lower pliocene | PELAGIC CLAYSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 0 | 98 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
199.40 | 60-453-22-1,40 | 3 | 27 | 70 | Lower pliocene | VITRIC MUDSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 69 | 0 | 0 | 0 | 2 | 0 | 0 | 20 | 0 | 1 |
199.50 | 60-453-22-1,50 | 0 | 10 | 90 | Lower pliocene | VITRIC MUDSTONE | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 1 |
199.83 | 60-453-22-1,83 | 10 | 70 | 20 | Lower pliocene | SILTY CRYSTAL VITRIC TUFF | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 20 | 0 | 0 | 0 | 1 | 0 | 0 | 50 | 0 | 0 |
200.70 | 60-453-22-2,20 | 0 | 30 | 70 | Lower pliocene | VITRIC MUD | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 |
201.42 | 60-453-22-2,92 | 0 | 20 | 80 | Lower pliocene | VITRIC MUD - MUD WITH VOLC. GLASS | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 |
201.49 | 60-453-22-2,99 | 5 | 60 | 35 | Lower pliocene | CRYSTAL VITRIC MUD | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 35 | 0 | 0 | 0 | 1 | 0 | 0 | 45 | 0 | 0 |
201.70 | 60-453-22-21,120 | 0 | 10 | 90 | Lower pliocene | VITRIC MUD (MUD W/VOLC.GLAS & NANNOS) | relative abundance | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 2 |
202.45 | 60-453-22-CC,5 | 0 | 50 | 50 | Lower pliocene | SILTY VITRIC TUFF | relative abundance | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 0 | 1 |
209.31 | 60-453-23-1,81 | 0 | 0 | 0 | Lower pliocene | CLAYSTONE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 10 | 90 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
209.31 | 60-453-23-1,81 | 0 | 10 | 90 | Lower pliocene | OPAQUE (BLACK LAYER) (FE-MN) | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 7 | 0 | 0 |
209.47 | 60-453-23-1,97 | 0 | 5 | 95 | Lower pliocene | CLAYSTONE (DARKER IN COLOR) | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 2 |
209.48 | 60-453-23-1,98 | 0 | 20 | 80 | Lower pliocene | MUDSTONE W/ABUNDANT GLASS, VITRIC MUD | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 1 |
218.20 | 60-453-24-1,20 | 0 | 30 | 70 | Lower pliocene | VITRIC MUDSTONE, RICH IN VOLC. GLASS | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 0 |
218.69 | 60-453-24-1,69 | 0 | 10 | 90 | Lower pliocene | VITRIC MUDSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 0 | 83 | 2 | 0 | 0 | 2 | 0 | 0 | 10 | 0 | 2 |
218.78 | 60-453-24-1,78 | 0 | 80 | 20 | Lower pliocene | SILTY VITRIC TUFF | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 75 | 0 | 1 |
218.82 | 60-453-24-1,82 | 0 | 35 | 65 | Lower pliocene | CRYSTAL VITRIC MUDSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 65 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 1 |
218.87 | 60-453-24-1,87 | 0 | 30 | 70 | Lower pliocene | CRYSTAL VITRIC MUDSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 1 |
219.00 | 60-453-24-11,100 | 2 | 50 | 48 | Lower pliocene | SILTY VITRIC MUDSTONE (W/ABUNT. GLASS) | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 45 | 1 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 1 |
219.53 | 60-453-24-2,3 | 10 | 30 | 60 | Lower pliocene | CRYSTAL-VITRIC MUDSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 35 | 0 | 1 |
219.87 | 60-453-24-2,37 | 0 | 5 | 95 | Lower pliocene | CLAYSTONE WITH NANNOS | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 90 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
219.98 | 60-453-24-2,48 | 5 | 35 | 60 | Lower pliocene | VITRIC MUDSTONE | numerical abundance | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 1 | 5 | 0 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 1 |
220.05 | 60-453-24-2,55 | 0 | 15 | 85 | Lower pliocene | VITRIC CRYSTAL MUDSTONE | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 85 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 |
220.25 | 60-453-24-2,75 | 0 | 20 | 80 | Lower pliocene | VITRIC CRYSTAL MUDSTONE | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 |
220.75 | 60-453-24-21,125 | 0 | 10 | 90 | Lower pliocene | MUDSTONE WITH NANNOS | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 |
221.39 | 60-453-24-CC,13 | 0 | 30 | 70 | Lower pliocene | VITRIC MUDSTONE | relative abundance | 1 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 65 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 1 |
228.36 | 60-453-25-1,86 | 3 | 80 | 17 | Lower pliocene | SILTY VITRIC TUFF | numerical abundance | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 10 | 0 | 0 | 0 | 1 | 0 | 0 | 79 | 0 | 1 |
239.17 | 60-453-26-2,67 | 0 | 8 | 92 | Lower pliocene | VITRIC CLAYSTONE | relative abundance | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 2 |
239.24 | 60-453-26-2,74 | 0 | 15 | 85 | Lower pliocene | VITRIC MUDSTONE | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 80 | 0 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 2 |
239.25 | 60-453-26-2,75 | 0 | 6 | 94 | Lower pliocene | CLAYSTONE | relative abundance | 1 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 1 |
239.57 | 60-453-26-21,107 | 0 | 7 | 93 | Lower pliocene | VITRIC CLAYSTONE | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 89 | 0 | 0 | 0 | 2 | 0 | 0 | 7 | 0 | 2 |
241.66 | 60-453-26-4,16 | 10 | 90 | 0 | Lower pliocene | VITRIC TUFF - PUMICE FRAGMENT | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 90 | 0 | 0 |
246.55 | 60-453-27-1,5 | 0 | 5 | 95 | Lower pliocene | CLAYSTONE | relative abundance | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 90 | 0 | 0 | 0 | 2 | 0 | 0 | 5 | 0 | 1 |
247.20 | 60-453-27-1,70 | 0 | 20 | 80 | Lower pliocene | VITRIC MUDSTONE | relative abundance | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 1 |
247.95 | 60-453-27-11,145 | 5 | 25 | 70 | Lower pliocene | VITRIC MUDSTONE | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 |
248.05 | 60-453-27-2,5 | 0 | 20 | 80 | Lower pliocene | VITRIC MUDSTONE | relative abundance | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 |
248.55 | 60-453-27-2,55 | 0 | 40 | 60 | Lower pliocene | VITRIC MUDSTONE | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 35 | 0 | 1 |
248.77 | 60-453-27-2,77 | 0 | 10 | 90 | Lower pliocene | CLAYSTONE | relative abundance | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 88 | 0 | 0 | 0 | 2 | 0 | 0 | 5 | 0 | 3 |
248.85 | 60-453-27-2,85 | 0 | 5 | 95 | Lower pliocene | CLAYSTONE | relative abundance | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 92 | 0 | 0 | 0 | 2 | 0 | 0 | 3 | 0 | 2 |
248.96 | 60-453-27-2,96 | 0 | 8 | 92 | Lower pliocene | CLAYSTONE | relative abundance | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 1 |
249.07 | 60-453-27-21,107 | 0 | 5 | 95 | Lower pliocene | CLAYSTONE | numerical abundance | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 88 | 0 | 0 | 0 | 0 | 0 | 0 | 7 | 0 | 2 |
249.55 | 60-453-27-3,5 | 0 | 15 | 85 | Lower pliocene | VITRIC MUDSTONE | relative abundance | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 2 |
250.15 | 60-453-27-3,65 | 3 | 60 | 37 | Lower pliocene | SILTY VITRIC TUFF | relative abundance | 2 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 30 | 0 | 0 | 0 | 1 | 0 | 0 | 60 | 0 | 1 |
256.03 | 60-453-28-1,3 | 0 | 10 | 90 | Lower pliocene | CLAYSTONE WITH NANNOS | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 7 | 0 | 0 |
256.81 | 60-453-28-1,81 | 0 | 15 | 85 | Lower pliocene | MUDSTONE WITH NANNOS AND VOLC. GLASS | relative abundance | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 1 |
257.74 | 60-453-28-2,24 | 0 | 30 | 70 | Lower pliocene | MUDSTONE RICH IN VOLC.GLAS & NANNOS | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 0 |
265.58 | 60-453-29-1,8 | 0 | 5 | 95 | Lower pliocene | CLAYSTONE | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
265.77 | 60-453-29-1,27 | 0 | 10 | 90 | Lower pliocene | CLAYSTONE | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 |
265.82 | 60-453-29-1,32 | 5 | 35 | 60 | Lower pliocene | CRYSTAL VITRIC MUDSTONE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 10 |
265.92 | 60-453-29-1,42 | 0 | 10 | 90 | Lower pliocene | CLAYSTONE WITH NANNOS | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 7 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 |
266.07 | 60-453-29-1,57 | 15 | 30 | 55 | Lower pliocene | CRYSTAL VITRIC MUDSTONE | relative abundance | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 15 |
266.40 | 60-453-29-1,90 | 0 | 5 | 95 | Lower pliocene | CLAYSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
266.64 | 60-453-29-11,114 | 30 | 30 | 50 | Lower pliocene | CRYSTAL VITRIC MUDSTONE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 10 |
267.56 | 60-453-29-2,56 | 50 | 40 | 10 | Lower pliocene | SANDY CRYSTAL VITRIC TUFF | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 10 | 0 | 0 | 0 | 1 | 0 | 0 | 30 | 0 | 30 |
269.05 | 60-453-29-3,55 | 0 | 7 | 93 | Lower pliocene | MUDSTONE | relative abundance | 1 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 3 |
271.22 | 60-453-29-41,122 | 2 | 70 | 28 | Lower pliocene | SILTY VITRIC TUFF | relative abundance | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 7 | 0 | 0 | 30 | 0 | 0 | 0 | 2 | 0 | 0 | 60 | 0 | 1 |
271.83 | 60-453-29-CC,17 | 2 | 58 | 40 | Lower pliocene | VITRIC MUDSTONE | relative abundance | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 60 | 0 | 0 | 0 | 2 | 0 | 0 | 30 | 0 | 1 |
275.04 | 60-453-30-1,4 | 0 | 2 | 98 | Lower pliocene | CLAYSTONE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 98 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
275.89 | 60-453-30-1,89 | 0 | 5 | 95 | Lower pliocene | CLAYSTONE | numerical abundance | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 92 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 1 |
286.80 | 60-453-31-2,80 | 0 | 7 | 93 | Lower pliocene | CLAYSTONE | numerical abundance | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 89 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 2 |
289.00 | 60-453-31-CC,0 | 0 | 5 | 95 | Lower pliocene | CLAYSTONE | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 1 | 0 | 92 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 |
295.74 | 60-453-32-2,24 | 30 | 30 | 40 | Lower pliocene | SANDY CRYSTAL VITRIC TUFF | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 40 | 0 | 0 | 0 | 10 | 0 | 0 | 35 | 0 | 1 |
295.91 | 60-453-32-2,41 | 5 | 30 | 65 | Lower pliocene | MUDSTONE RICH IN MICRONODULES | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 65 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 30 |
297.37 | 60-453-32-3,37 | 5 | 15 | 80 | Lower pliocene | MUDSTONE WITH MICRONODULES | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 3 | 0 | 77 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 |
298.18 | 60-453-32-CC,0 | 5 | 15 | 80 | Lower pliocene | MUDSTONE RICH IN MICRONODULES | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 1 | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 17 |
304.37 | 60-453-33-1,87 | 0 | 15 | 85 | Lower pliocene | VITRIC MUDSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 82 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 1 |
305.22 | 60-453-33-2,22 | 0 | 20 | 80 | Lower pliocene | VITRIC MUDSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 1 |
305.72 | 60-453-33-2,72 | 50 | 30 | 20 | Lower pliocene | SANDY VITRIC TUFF | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 20 | 0 | 0 | 0 | 1 | 0 | 0 | 70 | 0 | 1 |
306.53 | 60-453-33-3,3 | 0 | 5 | 95 | Lower pliocene | CLAYSTONE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 |
307.13 | 60-453-33-3,63 | 0 | 40 | 60 | Lower pliocene | VITRIC MUDSTONE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 |
308.11 | 60-453-33-4,11 | 0 | 20 | 80 | Lower pliocene | CRYSTAL VITRIC MUDSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 1 | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 1 |
308.68 | 60-453-33-CC,0 | 0 | 10 | 90 | Lower pliocene | VITRIC MUDSTONE | relative abundance | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 86 | 1 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 1 |
313.25 | 60-453-34-1,25 | 50 | 20 | 30 | Lower pliocene | CRYSTAL VITRIC MUDDY TUFF | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 |
314.07 | 60-453-34-11,107 | 0 | 5 | 95 | Lower pliocene | MUDSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 1 | 0 | 98 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
317.93 | 60-453-34-CC,15 | 0 | 5 | 95 | Lower pliocene | CLAYSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 |
324.60 | 60-453-35-2,60 | 50 | 30 | 20 | Lower pliocene | CRYSTAL VITRIC SANDY TUFF | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 13 | 0 | 0 | 20 | 0 | 0 | 0 | 2 | 0 | 0 | 65 | 0 | 0 |
324.69 | 60-453-35-2,69 | 50 | 30 | 20 | Lower pliocene | CRYSTAL VITRIC SANDY TUFF | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 1 | 0 | 20 | 0 | 0 | 0 | 1 | 0 | 0 | 50 | 0 | 1 |
325.26 | 60-453-35-21,126 | 5 | 30 | 65 | Lower pliocene | VITRIC CRYSTAL MUDDY TUFF | relative abundance | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 5 | 0 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 15 |
327.12 | 60-453-35-4,12 | 30 | 50 | 20 | Lower pliocene | CRYSTAL VITRIC MUDDY TUFF | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 |
332.15 | 60-453-36-1,15 | 5 | 75 | 20 | Lower pliocene | ZEOLITIC MUDSTONE | relative abundance | 3 | 0 | 0 | 2 | 2 | 0 | 0 | 2 | 0 | 1 | 70 | 0 | 15 | 0 | 0 | 0 | 2 | 0 | 0 | 5 | 0 | 2 |
332.58 | 60-453-36-1,58 | 0 | 10 | 90 | Lower pliocene | CALCAREOUS OR DOLOMITE CHALK | relative abundance | 95 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
332.91 | 60-453-36-1,91 | 0 | 5 | 95 | Lower pliocene | CRYSTAL CLAYSTONE | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
335.81 | 60-453-36-3,81 | 2 | 18 | 80 | Lower pliocene | CRYSTAL MUDSTONE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
335.84 | 60-453-36-3,84 | 0 | 5 | 95 | Lower pliocene | CLAYSTONE | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
336.44 | 60-453-36-31,144 | 0 | 5 | 95 | Lower pliocene | CRYSTAL CLAYSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 90 | 0 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 0 |
336.45 | 60-453-36-31,145 | 5 | 30 | 65 | Lower pliocene | CRYSTAL VITRIC MUDSTONE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 0 |
336.60 | 60-453-36-4,10 | 2 | 18 | 80 | Lower pliocene | VITRIC MUDSTONE | numerical abundance | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 5 | 0 | 75 | 0 | 0 | 0 | 1 | 0 | 0 | 10 | 0 | 5 |
336.91 | 60-453-36-4,41 | 2 | 15 | 83 | Lower pliocene | ZEOLITIC MUDSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 10 | 0 | 80 | 0 | 0 | 0 | 1 | 0 | 0 | 5 | 0 | 3 |
338.10 | 60-453-36-5,10 | 0 | 3 | 97 | Lower pliocene | CLAYSTONE | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
343.77 | 60-453-37-2,77 | 5 | 25 | 70 | Lower pliocene | CRYSTAL VITRIC MUDSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 65 | 0 | 0 | 0 | 1 | 0 | 0 | 20 | 0 | 1 |
343.82 | 60-453-37-2,82 | 0 | 10 | 90 | Lower pliocene | MUDSTONE | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 87 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 0 |
344.48 | 60-453-37-21,148 | 0 | 5 | 95 | Lower pliocene | CLAYSTONE | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
346.80 | 60-453-37-4,80 | 0 | 10 | 90 | Lower pliocene | MUDSTONE | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 87 | 0 | 0 | 0 | 1 | 0 | 0 | 8 | 0 | 0 |
347.55 | 60-453-37-5,5 | 1 | 39 | 60 | Lower pliocene | ZEOLITIC MUDSTONE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 49 | 0 | 0 | 0 | 1 | 0 | 0 | 10 | 0 | 10 |
347.86 | 60-453-37-5,36 | 1 | 19 | 80 | Lower pliocene | ZEOLITIC MUDSTONE | relative abundance | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 1 | 30 | 0 | 60 | 0 | 0 | 0 | 1 | 0 | 0 | 5 | 0 | 4 |
360.96 | 60-453-39-1,46 | 2 | 5 | 93 | Lower pliocene | CRYSTAL CLAYSTONE | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
361.40 | 60-453-39-1,90 | 0 | 2 | 98 | Lower pliocene | CLAYSTONE | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 3 | 0 | 97 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
361.50 | 60-453-39-11,100 | 0 | 5 | 95 | Lower pliocene | CLAYSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 1 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
362.25 | 60-453-39-2,25 | 0 | 5 | 95 | Lower pliocene | CLAYSTONE | relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 5 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 2 |
363.60 | 60-453-39-3,10 | 0 | 6 | 94 | Lower pliocene | CLAYSTONE | relative abundance | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 90 | 0 | 0 | 0 | 2 | 0 | 0 | 5 | 0 | 0 |
364.51 | 60-453-39-31,101 | 0 | 25 | 75 | Lower pliocene | VITRIC MUDSTONE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 10 | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 |
364.58 | 60-453-39-31,108 | 0 | 11 | 89 | Lower pliocene | CLAYSTONE | numerical abundance | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 10 | 0 | 81 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 1 |
364.58 | 60-453-39-31,108 | 0 | 5 | 95 | Lower pliocene | ZEOLITIC MUDSTONE | numerical abundance | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 92 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 |
364.60 | 60-453-39-31,110 | 2 | 40 | 58 | Lower pliocene | VITRIC MUDSTONE | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 30 | 0 | 5 |
364.70 | 60-453-39-31,120 | 0 | 2 | 98 | Lower pliocene | CLAYSTONE | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 1 |
365.97 | 60-453-39-4,97 | 20 | 60 | 20 | Lower pliocene | VITRIC CRYSTAL MUDDY TUFF | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 10 | 0 | 20 | 10 | 0 | 0 | 25 | 0 | 0 | 10 | 0 | 0 |
374.48 | 60-453-40-31,148 | 2 | 20 | 78 | Lower pliocene | VITRIC MUDSTONE | relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 1 |
379.70 | 60-453-41-1,20 | 55 | 39 | 60 | Lower pliocene | ZEOLITIC MUDSTONE | relative abundance | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 2 | 10 | 0 | 53 | 0 | 0 | 0 | 2 | 0 | 0 | 5 | 0 | 30 |
380.45 | 60-453-41-1,95 | 1 | 34 | 65 | Lower pliocene | ZEOLITIC MUDSTONE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 10 | 0 | 57 | 5 | 0 | 0 | 1 | 0 | 0 | 20 | 0 | 5 |
383.00 | 60-453-41-3,50 | 0 | 15 | 85 | Lower pliocene | CRYSTAL-VITRIC MUDSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 1 |
383.04 | 60-453-41-3,54 | 0 | 10 | 90 | Lower pliocene | MUDSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 88 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 1 |
389.35 | 60-453-42-1,35 | 0 | 20 | 80 | Lower pliocene | ZEOLITIC VITRIC CRYSTAL MUDSTONE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 5 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 |
390.00 | 60-453-42-11,100 | 0 | 30 | 70 | Lower pliocene | ZEOLITIC CRYSTAL VITRIC MUDSTONE | relative abundance | 0 | 0 | 1 | 0 | 1 | 1 | 0 | 0 | 0 | 10 | 5 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 0 |
390.48 | 60-453-42-11,148 | 2 | 25 | 73 | Lower pliocene | ZEOLITIC CRYSTAL MUDSTONE | relative abundance | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 7 | 10 | 0 | 70 | 0 | 0 | 0 | 5 | 0 | 0 | 3 | 0 | 5 |
390.73 | 60-453-42-2,23 | 10 | 25 | 65 | Lower pliocene | CRYSTAL VITRIC ZEOLITIC MUDSTONE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 15 | 0 | 60 | 0 | 0 | 0 | 5 | 0 | 0 | 10 | 0 | 2 |
391.79 | 60-453-42-21,129 | 0 | 5 | 95 | Lower pliocene | CLAYSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 95 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 |
392.05 | 60-453-42-CC,23 | 0 | 10 | 90 | Lower pliocene | ZEOLITIC CLAYSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 1 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
408.42 | 60-453-44-1,42 | 2 | 15 | 83 | Lower pliocene | ZEOLITIC VITRIC MUDSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 80 | 0 | 0 | 0 | 1 | 0 | 0 | 15 | 0 | 0 |
408.85 | 60-453-44-1,85 | 0 | 5 | 95 | Lower pliocene | ZEOLITIC VITRIC CLAYSTONE | relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 5 |
408.93 | 60-453-44-1,93 | 0 | 0 | 0 | Lower pliocene | PYRITE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
410.55 | 60-453-44-21,105 | 2 | 10 | 88 | Lower pliocene | MUDSTONE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 2 | 0 | 86 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
427.01 | 60-453-46-1,1 | 0 | 3 | 97 | Lower pliocene | CLAYSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
428.25 | 60-453-46-11,125 | 1 | 2 | 97 | Lower pliocene | CLAYSTONE | relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 5 | 0 | 91 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 2 |
436.75 | 60-453-47-1,25 | 0 | 10 | 90 | Lower pliocene | CLAYSTONE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 7 | 0 | 0 | 90 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 |
436.88 | 60-453-47-1,38 | 0 | 2 | 98 | Lower pliocene | CLAYSTONE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 98 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
438.19 | 60-453-47-2,19 | 1 | 5 | 94 | Lower pliocene | CLAYSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 94 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
439.47 | 60-453-47-21,147 | 5 | 7 | 88 | Lower pliocene | MUDSTONE | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 12 | 0 | 0 | 88 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
446.37 | 60-453-48-1,37 | 30 | 30 | 40 | Lower pliocene | SANDY VITRIC TUFF | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 |