de Vries, K G; Kobayashi, Kazuo (2005): Smear slide analysis of Hole 58-446A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230841
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
White, Stan; Waples, Douglas W; Sloan, Jon R; Okada, Hisatake; Nisterenko, G; Mizuno, Atsuyuki; Marsh, Nicholas G; Kinoshita, Hajimu; Fountain, David M; Echols, D J; Dick, H; Curtis, Doris M; Chamley, Hervè; deVries Klein, George; Kobayashi, Kazuo (1980): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, LVIII, 1183 pp, https://doi.org/10.2973/dsdp.proc.58.1980
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 24.700700 * Longitude: 132.774800
Date/Time Start: 1978-01-18T00:00:00 * Date/Time End: 1978-01-18T00:00:00
Minimum DEPTH, sediment/rock: 373.10 m * Maximum DEPTH, sediment/rock: 620.23 m
Event(s):
58-446A * Latitude: 24.700700 * Longitude: 132.774800 * Date/Time: 1978-01-18T00:00:00 * Elevation: -4952.0 m * Penetration: 628.5 m * Recovery: 117.5 m * Location: North Pacific/Philippine Sea/BASIN * Campaign: Leg58 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 28 cores; 256.5 m cored; 0 m drilled; 45.8 % 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 | Calcareous spicules | Calc spic | % | Smear slide analysis | ||
13 | Radiolarians | Rad | % | Smear slide analysis | ||
14 | Diatoms | Diatoms | % | 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 | Opaque minerals | Opaque | % | Smear slide analysis | ||
23 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
24 | Heavy minerals | HM | % | Smear slide analysis | ||
25 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
26 | Palagonite | Palagonite | % | Smear slide analysis | ||
27 | Rock fragments | Rock fragm | % | Smear slide analysis | ||
28 | Minerals | Minerals | % | Smear slide analysis | isotropic minerals | |
29 | Micronodules | Micronod | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
3244 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 Calc spic [%] | 13 Rad [%] | 14 Diatoms [%] | 15 Spiculae [%] | 16 Qz [%] | 17 Fsp [%] | 18 Zeo [%] | 19 Mica [%] | 20 Clay min [%] | 21 Glt [%] | 22 Opaque [%] | 23 Py [%] | 24 HM [%] | 25 Volc glass [%] | 26 Palagonite [%] | 27 Rock fragm [%] | 28 Minerals [%] | 29 Micronod [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
373.10 | 58-446A-1-11,110 | 1 | 2 | 97 | Eocene | CLAYEY CHALK | Minor lithology; relative abundance | 64 | 0 | 2 | 0 | 5 | 0 | 0 | 1 | 1 | 1 | 0 | 25 | 2 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 2 |
373.14 | 58-446A-1-11,114 | 2 | 7 | 91 | Eocene | CLAYEY NANNO MARL | Dominat lithology; relative abundance | 32 | 15 | 1 | 0 | 10 | 0 | 0 | 2 | 1 | 5 | 2 | 25 | 2 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 5 |
373.86 | 58-446A-1-2,36 | 40 | 50 | 10 | Eocene | VOLC ASH | Dominat lithology; numerical abundance | 0 | 0 | 2 | 0 | 5 | 0 | 0 | 1 | 1 | 5 | 0 | 10 | 0 | 0 | 0 | 0 | 75 | 0 | 0 | 0 | 1 |
374.10 | 58-446A-1-2,60 | 85 | 10 | 5 | Eocene | VOLC ASH | Dominat lithology; numerical abundance | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 1 | 1 | 0 | 1 | 5 | 1 | 0 | 0 | 2 | 88 | 0 | 0 | 0 | 0 |
374.65 | 58-446A-1-21,115 | 70 | 20 | 10 | Eocene | VOLC ASH | Dominat lithology; relative abundance | 0 | 0 | 1 | 0 | 5 | 0 | 0 | 1 | 1 | 0 | 2 | 10 | 2 | 0 | 0 | 1 | 88 | 0 | 0 | 0 | 2 |
375.78 | 58-446A-1-CC,0 | 2 | 2 | 96 | Eocene | CLAYEY NANNO CHALK | Dominat lithology; numerical abundance | 40 | 20 | 2 | 0 | 1 | 0 | 0 | 1 | 1 | 2 | 1 | 20 | 1 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 1 |
375.78 | 58-446A-1-CC,0 | 1 | 2 | 97 | Eocene | CLAYEY CHALK | Dominat lithology; relative abundance | 70 | 0 | 1 | 0 | 2 | 0 | 0 | 1 | 1 | 0 | 2 | 24 | 0 | 1 | 0 | 1 | 2 | 0 | 0 | 0 | 0 |
382.03 | 58-446A-2-1,53 | 80 | 10 | 10 | Eocene | ALTERED VOLC ASH | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 2 | 0 | 0 | 1 | 0 | 1 | 97 | 0 | 0 | 0 | 0 |
382.05 | 58-446A-2-1,55 | 30 | 20 | 50 | Eocene | ALTERED VOLCANIC ASH | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 1 | 2 | 2 | 20 | 2 | 2 | 0 | 1 | 67 | 0 | 0 | 0 | 3 |
382.20 | 58-446A-2-1,70 | 60 | 15 | 25 | Eocene | ALTERED VOLCANIC ASH | Dominat lithology; relative abundance | 2 | 1 | 0 | 0 | 3 | 2 | 0 | 2 | 1 | 0 | 1 | 15 | 0 | 1 | 0 | 2 | 70 | 0 | 0 | 0 | 1 |
384.25 | 58-446A-2-21,125 | 2 | 10 | 88 | Eocene | LIMESTONE | Dominat lithology; relative abundance | 74 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 0 | 20 | 2 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 |
384.45 | 58-446A-2-21,145 | 1 | 10 | 89 | Eocene | ZEOLITIC CLAYSTONE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 5 | 40 | 0 | 40 | 2 | 3 | 0 | 1 | 0 | 0 | 0 | 2 | 2 |
385.05 | 58-446A-2-CC,0 | 1 | 15 | 80 | Eocene | CHALK | Dominat lithology; numerical abundance | 80 | 3 | 1 | 0 | 0 | 0 | 0 | 1 | 1 | 2 | 2 | 10 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 2 |
385.05 | 58-446A-2-CC,0 | 5 | 5 | 94 | Eocene | ZEOLITIC CLAYSTONE | Minor lithology; relative abundance | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 35 | 0 | 50 | 0 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 2 |
391.20 | 58-446A-3-1,20 | 10 | 10 | 80 | Eocene | MUDSTONE | Dominat lithology; numerical abundance | 2 | 0 | 0 | 0 | 1 | 0 | 5 | 5 | 5 | 1 | 1 | 73 | 0 | 5 | 0 | 1 | 1 | 0 | 0 | 0 | 0 |
391.32 | 58-446A-3-1,32 | 0 | 0 | 0 | Eocene | ALT ASH | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 1 | 7 | 0 | 1 | 0 | 0 | 90 | 0 | 0 | 0 | 0 |
392.12 | 58-446A-3-11,112 | 0 | 0 | 0 | Eocene | CLAYEY ALT ASH | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 1 | 0 | 5 | 3 | 2 | 1 | 1 | 15 | 2 | 2 | 0 | 0 | 70 | 0 | 0 | 0 | 0 |
393.58 | 58-446A-3-21,108 | 0 | 5 | 95 | Eocene | CLAYSTONE | Dominat lithology; relative abundance | 1 | 2 | 0 | 0 | 2 | 0 | 1 | 3 | 2 | 1 | 2 | 86 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
393.88 | 58-446A-3-21,138 | 0 | 5 | 95 | Eocene | GLAUC CLAYSTONE | Dominat lithology; numerical abundance | 2 | 3 | 0 | 0 | 1 | 0 | 5 | 2 | 1 | 1 | 1 | 78 | 0 | 5 | 0 | 0 | 1 | 0 | 0 | 0 | 0 |
394.25 | 58-446A-3-3,25 | 0 | 5 | 95 | Eocene | CALC CLAYSTONE | Dominat lithology; numerical abundance | 20 | 5 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 1 | 2 | 63 | 1 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
412.17 | 58-446A-6-2,67 | 1 | 1 | 98 | CLAYSTONE | Dominat lithology; numerical abundance | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 93 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | |
413.22 | 58-446A-6-3,22 | 0 | 0 | 0 | CLAYSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 20 | 0 | 75 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | |
413.22 | 58-446A-6-3,22 | 1 | 1 | 98 | CLAYSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 5 | 0 | 80 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | |
413.22 | 58-446A-6-3,22 | 1 | 1 | 98 | CLAYSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 80 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | |
438.60 | 58-446A-9-1,10 | 2 | 9 | 89 | Lower eocene | CALCAREOUS MUDSTONE | Dominat lithology; numerical abundance | 10 | 10 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 0 | 7 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 2 |
438.67 | 58-446A-9-1,17 | 4 | 16 | 80 | Lower eocene | CALCAREOUS MUDSTONE | Dominat lithology; numerical abundance | 13 | 12 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 0 | 0 | 67 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 3 |
448.28 | 58-446A-10-1,28 | 100 | 0 | 0 | Lower eocene | ALTERED ASH | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 3 | 2 | 0 | 0 | 62 | 0 | 3 | 0 | 0 | 30 | 0 | 0 | 0 | 0 |
448.70 | 58-446A-10-1,70 | 100 | 0 | 0 | Lower eocene | VOLCANIC ASH | Dominat lithology; numerical abundance | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 3 | 0 | 0 | 64 | 0 | 5 | 0 | 0 | 20 | 0 | 0 | 0 | 0 |
448.96 | 58-446A-10-1,96 | 75 | 15 | 10 | Lower eocene | ALT ASH | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 2 | 1 | 1 | 2 | 15 | 0 | 2 | 0 | 1 | 61 | 0 | 0 | 0 | 0 |
449.05 | 58-446A-10-11,105 | 0 | 0 | 0 | Lower eocene | CALCAREOUS ALTERED ASH | Minor lithology; numerical abundance | 30 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 0 | 0 | 60 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
450.00 | 58-446A-10-2,50 | 0 | 0 | 0 | Lower eocene | VOLC ASH | Dominat lithology; numerical abundance | 15 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 75 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
450.10 | 58-446A-10-2,60 | 5 | 15 | 80 | Lower eocene | CLAYEY ZEOLINE | Dominat lithology; numerical abundance | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 69 | 1 | 20 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
450.35 | 58-446A-10-2,85 | 0 | 0 | 0 | Lower eocene | VOLCANIC ASH (CALCAREOUS) | Dominat lithology; numerical abundance | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 2 | 0 | 0 | 30 | 0 | 5 | 0 | 0 | 50 | 0 | 0 | 0 | 0 |
451.50 | 58-446A-10-3,50 | 65 | 20 | 15 | Lower eocene | VOLCANIC ASH | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 3 | 2 | 0 | 2 | 10 | 0 | 0 | 0 | 1 | 67 | 0 | 0 | 0 | 0 |
452.20 | 58-446A-10-31,120 | 0 | 0 | 0 | Lower eocene | VOLCANIC ASH | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 2 | 1 | 1 | 1 | 10 | 0 | 5 | 0 | 1 | 74 | 0 | 0 | 0 | 0 |
452.90 | 58-446A-10-4,40 | 0 | 0 | 0 | Lower eocene | ASH/ALT ASH | Dominat lithology; relative abundance | 2 | 2 | 0 | 0 | 0 | 0 | 2 | 2 | 1 | 0 | 1 | 10 | 0 | 0 | 0 | 1 | 83 | 0 | 0 | 0 | 0 |
453.90 | 58-446A-10-41,140 | 0 | 0 | 0 | Lower eocene | GLAUC ALT ASH | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 2 | 0 | 1 | 10 | 15 | 5 | 0 | 1 | 63 | 0 | 0 | 0 | 0 |
454.15 | 58-446A-10-5,15 | 0 | 0 | 0 | Lower eocene | ALT ASH | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 2 | 0 | 1 | 1 | 1 | 0 | 2 | 15 | 0 | 0 | 0 | 0 | 81 | 0 | 0 | 0 | 0 |
454.35 | 58-446A-10-5,35 | 0 | 0 | 0 | Lower eocene | ALT ASH | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 2 | 0 | 1 | 1 | 1 | 2 | 3 | 15 | 0 | 3 | 0 | 0 | 78 | 0 | 0 | 0 | 0 |
454.65 | 58-446A-10-5,65 | 0 | 25 | 75 | Lower eocene | MUDSTONE | Dominat lithology; numerical abundance | 1 | 5 | 0 | 0 | 0 | 0 | 0 | 3 | 2 | 5 | 2 | 74 | 0 | 7 | 0 | 1 | 0 | 0 | 0 | 0 | 0 |
469.90 | 58-446A-12-21,140 | 2 | 28 | 70 | Lower eocene | FELDSPATHIC MUDSTONE | Dominat lithology; numerical abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 0 | 66 | 0 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 |
469.92 | 58-446A-12-21,142 | 1 | 26 | 73 | Lower eocene | MUDSTONE | Dominat lithology; numerical abundance | 7 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 4 | 0 | 73 | 0 | 3 | 0 | 1 | 2 | 0 | 0 | 0 | 0 |
469.95 | 58-446A-12-21,145 | 1 | 18 | 81 | Lower eocene | CLAYEY MUDSTONE | Dominat lithology; numerical abundance | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 4 | 0 | 80 | 0 | 2 | 0 | 2 | 1 | 0 | 0 | 0 | 0 |
470.16 | 58-446A-12-3,16 | 1 | 9 | 90 | Lower eocene | CLAYSTONE | Minor lithology; numerical abundance | 5 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 87 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 |
470.60 | 58-446A-12-3,60 | 15 | 65 | 20 | Lower eocene | CLAYEY ASHY,SILTSTONE | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 20 | 0 | 0 | 0 | 2 | 68 | 0 | 0 | 0 | 0 |
471.10 | 58-446A-12-31,110 | 1 | 24 | 75 | Lower eocene | ASHY MUDSTONE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 76 | 0 | 1 | 0 | 1 | 20 | 0 | 0 | 0 | 0 |
471.55 | 58-446A-12-4,5 | 7 | 63 | 30 | Lower eocene | ASHY SILTY MUDSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 30 | 0 | 5 | 0 | 2 | 62 | 0 | 0 | 0 | 0 |
479.67 | 58-446A-13-3,17 | 8 | 30 | 62 | Lower eocene | ASHY MUDSTONE | Dominat lithology; numerical abundance | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 55 | 0 | 3 | 0 | 2 | 30 | 0 | 0 | 0 | 0 |
480.25 | 58-446A-13-3,75 | 15 | 50 | 35 | Lower eocene | ASHY CLAYEY SILTSTONE | Dominat lithology; numerical abundance | 4 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 40 | 0 | 4 | 0 | 4 | 40 | 0 | 0 | 0 | 0 |
480.45 | 58-446A-13-3,95 | 20 | 63 | 17 | Lower eocene | VOLCANIC SILTSTONE | Dominat lithology; numerical abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 17 | 0 | 10 | 0 | 2 | 67 | 0 | 0 | 0 | 0 |
480.90 | 58-446A-13-31,140 | 15 | 50 | 35 | Lower eocene | ASHY SILTY MUDSTONE | Dominat lithology; numerical abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 35 | 0 | 5 | 0 | 2 | 53 | 0 | 0 | 0 | 0 |
481.33 | 58-446A-13-CC,0 | 50 | 20 | 15 | Lower eocene | CALC SANDSTONE | Dominat lithology; numerical abundance | 15 | 10 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 1 | 1 | 26 | 5 | 5 | 0 | 1 | 1 | 0 | 5 | 0 | 0 |
481.33 | 58-446A-13-CC,0 | 65 | 38 | 15 | Lower eocene | GLAUCONITIC CLAYSTONE | Dominat lithology; numerical abundance | 5 | 5 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 1 | 2 | 88 | 0 | 5 | 0 | 0 | 20 | 0 | 0 | 0 | 0 |
486.10 | 58-446A-14-1,10 | 5 | 25 | 70 | Lower eocene | PYRITE MANGANESE GLAUCONITE MUDSTONE | Dominat lithology; relative abundance | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 5 | 0 | 0 | 70 | 7 | 3 | 10 | 1 | 0 | 0 | 0 | 0 | 5 |
486.14 | 58-446A-14-1,14 | 10 | 65 | 10 | Lower eocene | GLAUCONITIC MUDSTONE | Dominat lithology; numerical abundance | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 25 | 25 | 0 | 2 | 10 | 15 | 5 | 0 | 10 | 0 | 0 | 10 | 0 | 0 |
486.14 | 58-446A-14-1,14 | 25 | 75 | 15 | Lower eocene | SANDY MUDSTONE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 35 | 0 | 0 | 18 | 15 | 5 | 0 | 5 | 0 | 0 | 10 | 0 | 0 |
508.65 | 58-446A-16-3,65 | 35 | 50 | 15 | Lower eocene | SANDY ASH | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 35 | 0 | 0 | 11 | 0 | 0 | 0 | 5 | 45 | 0 | 0 | 0 | 2 |
509.35 | 58-446A-16-31,135 | 40 | 50 | 10 | Lower eocene | SANDY ASH | Dominat lithology; relative abundance | 0 | 0 | 0 | 2 | 5 | 0 | 0 | 0 | 25 | 0 | 0 | 5 | 2 | 1 | 0 | 0 | 60 | 0 | 0 | 0 | 2 |
510.25 | 58-446A-16-4,75 | 50 | 50 | 0 | Lower eocene | ASH | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 95 | 0 | 0 | 0 | 0 |
511.20 | 58-446A-16-5,20 | 40 | 50 | 10 | Lower eocene | SANDY ASH | Dominat lithology; numerical abundance | 0 | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 25 | 0 | 0 | 10 | 0 | 1 | 0 | 2 | 60 | 0 | 0 | 0 | 0 |
511.54 | 58-446A-16-CC,0 | 1 | 40 | 20 | Lower eocene | CALCAREOUS MUDSTONE | Dominat lithology; numerical abundance | 10 | 0 | 10 | 0 | 2 | 0 | 0 | 0 | 10 | 2 | 0 | 13 | 1 | 2 | 0 | 5 | 50 | 0 | 0 | 0 | 10 |
511.54 | 58-446A-16-CC,0 | 30 | 50 | 59 | Lower eocene | SANDY ASH | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 25 | 5 | 0 | 50 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 |
514.93 | 58-446A-17-1,43 | 7 | 20 | 73 | Lower eocene | ALTERED ASH | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 1 | 0 | 2 | 10 | 10 | 0 | 0 | 73 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 5 |
515.63 | 58-446A-17-11,113 | 2 | 31 | 67 | Lower eocene | CALCAREOUS MUDSTONE | Dominat lithology; numerical abundance | 20 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 1 | 0 | 0 | 67 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 |
515.75 | 58-446A-17-11,125 | 2 | 8 | 90 | Lower eocene | CALCAREOUS MUDSTONE | Minor lithology; numerical abundance | 35 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 0 | 61 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
515.80 | 58-446A-17-11,130 | 10 | 27 | 63 | Lower eocene | CALCAREOUS MUDSTONE (SILICEOUS) | Dominat lithology; numerical abundance | 30 | 0 | 0 | 0 | 10 | 0 | 0 | 3 | 2 | 0 | 0 | 53 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
516.95 | 58-446A-17-2,95 | 8 | 22 | 70 | Lower eocene | CALCAREOUS MUDSTONE | Dominat lithology; relative abundance | 15 | 0 | 0 | 0 | 1 | 0 | 0 | 8 | 7 | 0 | 2 | 63 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 |
517.95 | 58-446A-17-3,45 | 0 | 30 | 70 | Lower eocene | CALCAREOUS ASHY MUDSTONE | Dominat lithology; numerical abundance | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 2 | 0 | 0 | 67 | 1 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 7 |
518.29 | 58-446A-17-CC,0 | 0 | 5 | 95 | Lower eocene | ZEOLITIC CLAYSTONE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 10 | 0 | 80 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 2 |
524.15 | 58-446A-18-1,15 | 1 | 39 | 60 | Lower eocene | VITRIC CALCAREOUS MUDSTONE | Dominat lithology; relative abundance | 15 | 0 | 0 | 0 | 2 | 0 | 0 | 4 | 4 | 0 | 0 | 56 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 6 |
524.50 | 58-446A-18-1,50 | 0 | 0 | 0 | Lower eocene | CALCAREOUS MUDSTONE | Dominat lithology; numerical abundance | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 7 |
524.95 | 58-446A-18-1,95 | 40 | 50 | 10 | Lower eocene | CALCAREOUS SANDY MUDSTONE | Minor lithology; numerical abundance | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 10 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 |
525.29 | 58-446A-18-11,129 | 0 | 0 | 0 | Lower eocene | CHALK | Dominat lithology; numerical abundance | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
525.79 | 58-446A-18-2,29 | 0 | 9 | 91 | Lower eocene | CLAYSTONE | Dominat lithology; numerical abundance | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 2 | 0 | 0 | 86 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 |
526.00 | 58-446A-18-2,50 | 5 | 15 | 80 | Lower eocene | GLAUCONITIC CALCAREOUS MUDSTONE | Minor lithology; numerical abundance | 6 | 6 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 0 | 76 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
535.20 | 58-446A-19-2,20 | 7 | 18 | 75 | Lower eocene | GLAUCONITE MUDSTONE | Dominat lithology; relative abundance | 2 | 2 | 0 | 0 | 15 | 0 | 0 | 1 | 1 | 0 | 0 | 75 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
536.65 | 58-446A-19-3,15 | 1 | 15 | 84 | Lower eocene | GLAUC CLAYSTONE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 1 | 0 | 72 | 20 | 5 | 0 | 0 | 1 | 0 | 0 | 0 | 0 |
536.70 | 58-446A-19-3,20 | 0 | 25 | 0 | Lower eocene | MUDSTONE | Dominat lithology; relative abundance | 2 | 2 | 0 | 0 | 0 | 0 | 5 | 2 | 1 | 1 | 1 | 69 | 7 | 10 | 0 | 1 | 1 | 0 | 0 | 0 | 0 |
562.42 | 58-446A-22-1,42 | 20 | 30 | 50 | Lower eocene | VITRIC MUDSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 0 | 10 | 0 | 1 | 15 | 3 | 2 | 0 | 5 | 30 | 0 | 5 | 0 | 0 |
562.45 | 58-446A-22-1,45 | 0 | 5 | 95 | Lower eocene | CLAYSTONE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 1 | 0 | 87 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 |
562.66 | 58-446A-22-1,66 | 40 | 40 | 20 | Lower eocene | ALTERED VOLCANIC ASH | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 1 | 0 | 3 | 0 | 10 | 0 | 0 | 22 | 1 | 0 | 0 | 2 | 60 | 0 | 0 | 0 | 1 |
562.73 | 58-446A-22-1,73 | 30 | 30 | 40 | Lower eocene | ALTERED VOLCANIC ASH | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 2 | 0 | 3 | 0 | 10 | 2 | 0 | 35 | 5 | 0 | 0 | 3 | 30 | 0 | 0 | 0 | 10 |
562.93 | 58-446A-22-1,93 | 10 | 15 | 75 | Lower eocene | SANDY MUDSTONE | Dominat lithology; relative abundance | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 2 | 1 | 1 | 84 | 1 | 7 | 0 | 1 | 0 | 0 | 0 | 0 | 0 |
563.00 | 58-446A-22-11,100 | 1 | 30 | 69 | Lower eocene | MUDSTONE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 2 | 1 | 44 | 3 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 20 |
563.21 | 58-446A-22-11,121 | 1 | 4 | 95 | Lower eocene | CLAYSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 2 | 50 | 5 | 3 | 0 | 10 | 0 | 0 | 2 | 0 | 20 |
563.24 | 58-446A-22-11,124 | 0 | 5 | 95 | Lower eocene | CLAYSTONE WITH ALTERED FELDSPAR | Dominat lithology; relative abundance | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 2 | 65 | 2 | 5 | 0 | 5 | 0 | 0 | 0 | 0 | 0 |
563.28 | 58-446A-22-11,128 | 1 | 20 | 79 | Lower eocene | CLAYEY MUDSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 50 | 2 | 2 | 35 | 2 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 3 |
571.76 | 58-446A-23-1,26 | 1 | 28 | 71 | Lower eocene | MUDSTONE | Dominat lithology; relative abundance | 1 | 2 | 0 | 0 | 8 | 0 | 0 | 5 | 5 | 0 | 0 | 71 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 7 |
571.83 | 58-446A-23-1,33 | 3 | 80 | 17 | Lower eocene | GLAUCONITE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 92 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 |
572.30 | 58-446A-23-1,80 | 2 | 7 | 91 | Lower eocene | CLAYSTONE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 1 | 1 | 0 | 0 | 91 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 |
572.63 | 58-446A-23-11,113 | 2 | 12 | 86 | Lower eocene | RAD-RICH MUDSTONE | Dominat lithology; relative abundance | 0 | 2 | 0 | 0 | 7 | 0 | 0 | 1 | 1 | 0 | 0 | 86 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 |
581.30 | 58-446A-24-1,30 | 3 | 19 | 78 | Lower eocene | GLAUCONITIC MUDSTONE | Dominat lithology; relative abundance | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 0 | 78 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
581.68 | 58-446A-24-1,68 | 1 | 31 | 68 | Lower eocene | GLAUCONITIC MUDSTONE | Dominat lithology; relative abundance | 0 | 2 | 0 | 0 | 4 | 0 | 0 | 2 | 1 | 0 | 0 | 68 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 |
581.80 | 58-446A-24-1,80 | 0 | 18 | 82 | Lower eocene | MUDSTONE | Dominat lithology; relative abundance | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 4 | 3 | 0 | 0 | 82 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 7 |
581.90 | 58-446A-24-1,90 | 3 | 20 | 77 | Lower eocene | GLAUCONITIC MUDSTONE | Minor lithology; relative abundance | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 0 | 77 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 |
582.10 | 58-446A-24-11,110 | 0 | 21 | 79 | Lower eocene | MUDSTONE | Dominat lithology; relative abundance | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 0 | 0 | 79 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 15 |
582.95 | 58-446A-24-2,45 | 0 | 27 | 83 | Lower eocene | MUDSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 4 | 0 | 0 | 75 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 13 |
594.42 | 58-446A-25-3,92 | 1 | 19 | 80 | Lower eocene | FELDSPAR RICH MUDSTONE | Dominat lithology; numerical abundance | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 79 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 |
594.48 | 58-446A-25-3,98 | 0 | 20 | 80 | Lower eocene | ZEOLITIC MUDSTONE | Minor lithology; numerical abundance | 8 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 15 | 0 | 70 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
594.62 | 58-446A-25-31,112 | 1 | 1 | 98 | Lower eocene | CLAYEY NANNO CHALK | Dominat lithology; numerical abundance | 15 | 35 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 48 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
594.97 | 58-446A-25-31,147 | 10 | 40 | 50 | Lower eocene | ASHY MUDSTONE | Dominat lithology; numerical abundance | 3 | 1 | 0 | 0 | 5 | 0 | 0 | 0 | 6 | 0 | 1 | 40 | 3 | 5 | 0 | 2 | 33 | 1 | 0 | 0 | 0 |
595.35 | 58-446A-25-4,35 | 10 | 35 | 55 | Lower eocene | ASHY MUDSTONE W/SILICEOUS FOSSILS | Dominat lithology; numerical abundance | 1 | 0 | 0 | 0 | 9 | 0 | 2 | 0 | 8 | 0 | 5 | 48 | 0 | 5 | 0 | 0 | 20 | 2 | 0 | 0 | 0 |
595.78 | 58-446A-25-4,78 | 10 | 35 | 55 | Lower eocene | ASHY MUDSTONE W/MICRONODULES | Dominat lithology; numerical abundance | 3 | 2 | 0 | 0 | 3 | 0 | 0 | 0 | 8 | 0 | 5 | 44 | 2 | 0 | 0 | 2 | 20 | 1 | 0 | 0 | 10 |
600.01 | 58-446A-26-1,1 | 5 | 40 | 55 | Lower eocene | GLAUCONITIC MUDSTONE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 44 | 40 | 15 | 0 | 2 | 0 | 0 | 0 | 0 | 0 |
600.03 | 58-446A-26-1,3 | 1 | 29 | 70 | Lower eocene | FELDSPAR-RICH MUDSTONE | Minor lithology; numerical abundance | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 69 | 3 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 |
603.60 | 58-446A-26-3,60 | 35 | 50 | 15 | Lower eocene | GLAUCONITIC SANDY SILTSTONE | Minor lithology; numerical abundance | 4 | 1 | 0 | 0 | 3 | 0 | 0 | 0 | 3 | 0 | 0 | 14 | 0 | 0 | 0 | 2 | 72 | 1 | 0 | 0 | 0 |
603.80 | 58-446A-26-3,80 | 9 | 41 | 50 | Lower eocene | ASHY GLAUCONITIC SILTY MUDSTONE | Dominat lithology; relative abundance | 10 | 0 | 0 | 0 | 9 | 0 | 0 | 0 | 3 | 0 | 2 | 17 | 45 | 0 | 0 | 1 | 15 | 0 | 0 | 0 | 0 |
603.95 | 58-446A-26-3,95 | 1 | 29 | 70 | Lower eocene | CALCAREOUS GLAUCONITIC CLAYEY MUDSTONE | Dominat lithology; relative abundance | 12 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 1 | 0 | 3 | 56 | 20 | 0 | 0 | 2 | 5 | 0 | 0 | 0 | 0 |
604.03 | 58-446A-26-31,103 | 1 | 9 | 90 | Lower eocene | CLAYSTONE | Minor lithology; numerical abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 4 | 0 | 89 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 |
612.46 | 58-446A-27-21,146 | 0 | 2 | 95 | Lower eocene | CALCAREOUS CLAYSTONE | Dominat lithology; relative abundance | 25 | 2 | 2 | 0 | 4 | 0 | 0 | 1 | 1 | 1 | 2 | 18 | 2 | 0 | 0 | 1 | 2 | 0 | 0 | 0 | 4 |
612.46 | 58-446A-27-21,146 | 0 | 2 | 98 | Lower eocene | CHALKY CLAYSTONE | Dominat lithology; relative abundance | 34 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 1 | 0 | 43 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 4 |
612.46 | 58-446A-27-21,146 | 0 | 2 | 98 | Lower eocene | CHALKY CLAYSTONE W/RADS | Dominat lithology; relative abundance | 39 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 1 | 0 | 50 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 8 |
612.46 | 58-446A-27-21,146 | 0 | 5 | 98 | Lower eocene | CLAYEY CHALK | Dominat lithology; relative abundance | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 59 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 |
619.82 | 58-446A-28-1,82 | 7 | 46 | 47 | Lower eocene | ALTERED ASH | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 7 | 0 | 3 | 0 | 7 | 0 | 0 | 0 | 75 | 0 | 0 | 0 | 0 |
619.90 | 58-446A-28-1,90 | 1 | 44 | 55 | Lower eocene | GLAUCONITIC MUDSTONE | Dominat lithology; numerical abundance | 4 | 3 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 0 | 51 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 |
620.23 | 58-446A-28-11,123 | 0 | 35 | 65 | Lower eocene | GLAUCONITIC MUDSTONE | Dominat lithology; numerical abundance | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 1 | 64 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 |