Worzel, J Lamar; Bryant, William (2005): Smear slide analysis of Hole 10-85. PANGAEA, https://doi.org/10.1594/PANGAEA.230309
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
Smith, L A; McNeely, B; Laury, R; Foreman, H P; Dickinson, K; Capo, R; Beall, A O; Worzel, J Lamar; Bryant, William (1973): Initial Reports of the Deep Sea Drilling Project 10. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, X, 748 pp, https://doi.org/10.2973/dsdp.proc.10.1973
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 22.841500 * Longitude: -91.422800
Date/Time Start: 1970-02-21T00:00:00 * Date/Time End: 1970-02-21T00:00:00
Minimum DEPTH, sediment/rock: 19.39 m * Maximum DEPTH, sediment/rock: 212.30 m
Event(s):
10-85 * Latitude: 22.841500 * Longitude: -91.422800 * Date/Time: 1970-02-21T00:00:00 * Elevation: -3749.0 m * Penetration: 212.6 m * Recovery: 26.5 m * Location: Gulf of Mexico/PLAIN * Campaign: Leg10 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 5 cores; 38.6 m cored; 0 m drilled; 68.7 % 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 | Aragonite | Arg | % | Smear slide analysis | ||
12 | Nannofossils | Nannos | % | Smear slide analysis | ||
13 | Foraminifera | Foram | % | Smear slide analysis | ||
14 | Chert | Chert | % | Smear slide analysis | fragments | |
15 | Radiolarians | Rad | % | Smear slide analysis | ||
16 | Diatoms | Diatoms | % | Smear slide analysis | ||
17 | Spiculae | Spiculae | % | Smear slide analysis | ||
18 | Quartz | Qz | % | Smear slide analysis | ||
19 | Feldspar | Fsp | % | Smear slide analysis | ||
20 | Zeolite | Zeo | % | Smear slide analysis | ||
21 | Mica | Mica | % | Smear slide analysis | ||
22 | Biotite | Bt | % | Smear slide analysis | ||
23 | Glauconite | Glt | % | Smear slide analysis | ||
24 | Opaque minerals | Opaque | % | Smear slide analysis | ||
25 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
26 | Heavy minerals | HM | % | Smear slide analysis | ||
27 | Zircon | Zrn | % | Smear slide analysis | ||
28 | Tourmaline | Tur | % | Smear slide analysis | ||
29 | Apatite | Ap | % | Smear slide analysis | ||
30 | Amphibole | Amp | % | Smear slide analysis | ||
31 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
32 | Fragments | Fragm | % | Smear slide analysis | calcareous material | |
33 | Basalt | Basalt | % | Smear slide analysis | ||
34 | Fecal pellets | Fecal pel | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
891 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 Arg [%] | 12 Nannos [%] | 13 Foram [%] | 14 Chert [%] | 15 Rad [%] | 16 Diatoms [%] | 17 Spiculae [%] | 18 Qz [%] | 19 Fsp [%] | 20 Zeo [%] | 21 Mica [%] | 22 Bt [%] | 23 Glt [%] | 24 Opaque [%] | 25 Py [%] | 26 HM [%] | 27 Zrn [%] | 28 Tur [%] | 29 Ap [%] | 30 Amp [%] | 31 Volc glass [%] | 32 Fragm [%] | 33 Basalt [%] | 34 Fecal pel [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
19.39 | 10-85-1-1,20 | 10 | 40 | 60 | Upper pleistocene | QUARTZOSE MUD | Dominat lithology; relative abundance | 15 | 2 | 0 | 23 | 6 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 6 |
19.78 | 10-85-1-1,59 | 10 | 60 | 85 | Upper pleistocene | FORAMINIFERAL NANNO OOZE | Dominat lithology; relative abundance | 36 | 0 | 2 | 23 | 10 | 0 | 0 | 0 | 3 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 |
20.89 | 10-85-1-2,20 | 10 | 50 | 60 | Upper pleistocene | QUARTZOSE MUD | Dominat lithology; relative abundance | 10 | 2 | 2 | 6 | 6 | 0 | 2 | 0 | 0 | 55 | 2 | 0 | 2 | 0 | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
22.23 | 10-85-1-3,4 | 0 | 35 | 60 | Upper pleistocene | MUD | Dominat lithology; relative abundance | 15 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 2 | 55 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 2 | 0 | 0 | 0 |
22.39 | 10-85-1-3,20 | 1 | 60 | 60 | Upper pleistocene | NANNO OOZE | Dominat lithology; relative abundance | 30 | 0 | 2 | 23 | 6 | 0 | 0 | 0 | 6 | 2 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 |
23.19 | 10-85-1-31,100 | 0 | 60 | 85 | Upper pleistocene | CALCAREOUS CLAY (TERRIGENOUS MUD) | Dominat lithology; relative abundance | 15 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 |
23.73 | 10-85-1-4,4 | 0 | 60 | 60 | Upper pleistocene | TERRIGENOUS MUD | Dominat lithology; relative abundance | 20 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 23 | 0 | 6 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
24.80 | 10-85-1-41,111 | 0 | 60 | 60 | Upper pleistocene | SLIGHTLY CALCAREOUS MUD | Dominat lithology; relative abundance | 0 | 0 | 0 | 6 | 6 | 0 | 0 | 2 | 0 | 6 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 23 |
25.34 | 10-85-1-5,15 | 0 | 60 | 60 | Upper pleistocene | QUARTZOSE MUD | Dominat lithology; relative abundance | 15 | 2 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 55 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 6 | 0 | 0 | 0 |
25.92 | 10-85-1-5,73.5 | 35 | 60 | 60 | Upper pleistocene | FORAM NANNO OOZE | Dominat lithology; relative abundance | 50 | 0 | 6 | 23 | 23 | 0 | 0 | 0 | 6 | 23 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
26.72 | 10-85-1-6,3 | 0 | 60 | 60 | Upper pleistocene | NANNO-BEARING QUARTZOSE SILTY MUD | Dominat lithology; relative abundance | 14 | 4 | 0 | 16 | 2 | 0 | 0 | 0 | 0 | 39 | 2 | 3 | 18 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 |
27.10 | 10-85-1-6,41 | 0 | 60 | 60 | Upper pleistocene | NANNO OOZE | Dominat lithology; relative abundance | 60 | 0 | 6 | 23 | 0 | 0 | 0 | 2 | 6 | 6 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 6 | 0 | 0 | 0 |
27.40 | 10-85-1-6,71 | 0 | 60 | 60 | Upper pleistocene | TERRIGENOUS MUD | Dominat lithology; relative abundance | 60 | 2 | 0 | 6 | 2 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 |
48.02 | 10-85-2-1,2 | 60 | 60 | 60 | Upper pleistocene | NANNO-BEARING MUDDY SAND | Dominat lithology; relative abundance | 8 | 3 | 0 | 12 | 3 | 0 | 0 | 3 | 3 | 40 | 3 | 0 | 6 | 0 | 2 | 12 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
49.52 | 10-85-2-2,2 | 85 | 35 | 35 | Upper pleistocene | FORAM-BEARING FINE TO VERY FINE SAND | Dominat lithology; relative abundance | 5 | 15 | 0 | 0 | 15 | 0 | 0 | 0 | 4 | 49 | 4 | 0 | 8 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
49.69 | 10-85-2-2,19 | 0 | 60 | 85 | Upper pleistocene | TERRIGENOUS MUD | Dominat lithology; relative abundance | 10 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
51.02 | 10-85-2-3,2 | 10 | 60 | 60 | Upper pleistocene | TERRIGENOUS MUD | Dominat lithology; relative abundance | 15 | 2 | 0 | 23 | 2 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
100.52 | 10-85-3-2,2 | 10 | 60 | 60 | Upper pleistocene | TERRIGENOUS MUD | Dominat lithology; relative abundance | 10 | 2 | 0 | 6 | 2 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
100.60 | 10-85-3-2,10 | 10 | 60 | 85 | Upper pleistocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 40 | 0 | 0 | 37 | 15 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 |
102.04 | 10-85-3-3,4 | 0 | 60 | 85 | Upper pleistocene | CALCAREOUS MUD | Dominat lithology; relative abundance | 50 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 0 |
106.54 | 10-85-3-6,4 | 0 | 35 | 60 | Upper pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 18 | 14 | 0 | 32 | 0 | 0 | 0 | 0 | 0 | 32 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
189.14 | 10-85-4-1,4 | 10 | 35 | 85 | Upper pleistocene | SILTY NANNO OOZE | Dominat lithology; numerical abundance | 28 | 3 | 0 | 42 | 3 | 3 | 0 | 0 | 0 | 13 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 3 |
189.76 | 10-85-4-1,66 | 10 | 35 | 85 | Upper pleistocene | SILTY NANNO OOZE (CALCILUTITE) (TERRIGENOUS MUD) | Dominat lithology; relative abundance | 30 | 0 | 0 | 55 | 2 | 6 | 0 | 0 | 0 | 6 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 1 |
190.23 | 10-85-4-11,113 | 10 | 35 | 60 | Upper pleistocene | NANNO OOZE | Dominat lithology; relative abundance | 40 | 0 | 0 | 40 | 12 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 3 |
190.35 | 10-85-4-11,125 | 35 | 35 | 60 | Upper pleistocene | CALCAREOUS NANNO MUD (CALCUCITE)(OOZE) | Dominat lithology; relative abundance | 41 | 3 | 0 | 42 | 3 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 4 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 1 |
190.50 | 10-85-4-11,140 | 10 | 60 | 60 | Upper pleistocene | NANNO AND DOLOMITE-BEARING SILTY MUD | Dominat lithology; relative abundance | 30 | 55 | 0 | 24 | 0 | 6 | 0 | 0 | 0 | 6 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 6 | 6 |
212.30 | 10-85-5-2,80 | 85 | 10 | 0 | Upper pleistocene | POLYCYCLIC (ORTHO) MEDIUM FINE SAND WITH VOLCANOGENIC COMPONENT | Dominat lithology; relative abundance | 9 | 4 | 0 | 4 | 4 | 4 | 0 | 0 | 0 | 45 | 14 | 0 | 4 | 0 | 0 | 0 | 1 | 0 | 2 | 4 | 2 | 4 | 0 | 0 | 4 | 0 |