Honnorez, Jose J; von Herzen, Richard P (2005): Smear slide analysis of Hole 70-507C [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230996
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
Schrader, Ed L; Moorby, S A; Migdisov, Areg A; Levi, Shaul; Laverne, Christine; Karato, Shun-ichiro; Jones, S C; Hubberten, Hans-Wolfgang; Bender, Michael L; Becker, Keir; Barrett, T J; Borella, Peter E; Honnorez, Jose J; von Herzen, Richard P (1983): Initial Reports of the Deep Sea Drilling Project. U.S. Government Printing Office, LXX, 481 pp, https://doi.org/10.2973/dsdp.proc.70.1983
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 0.566700 * Longitude: -86.090000
Date/Time Start: 1979-11-20T00:00:00 * Date/Time End: 1979-11-20T00:00:00
Minimum DEPTH, sediment/rock: 0.03 m * Maximum DEPTH, sediment/rock: 8.18 m
Event(s):
70-507C * Latitude: 0.566700 * Longitude: -86.090000 * Date/Time: 1979-11-20T00:00:00 * Elevation: -2710.0 m * Penetration: 29.5 m * Recovery: 9.2 m * Location: North Pacific/MOUND * Campaign: Leg70 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 4 cores; 43 m cored; 0 m drilled; 21.3 % recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Sample code/label | Sample label | DSDP/ODP/IODP sample designation | |||
| 3 | Sand | Sand | % | Smear slide analysis | ||
| 4 | Silt | Silt | % | Smear slide analysis | ||
| 5 | Size fraction < 0.002 mm, clay | <2 µm | % | Smear slide analysis | ||
| 6 | 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 | Clay minerals | Clay min | % | Smear slide analysis | ||
| 16 | Glauconite | Glt | % | Smear slide analysis | ||
| 17 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
| 18 | Micronodules | Micronod | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
118 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 Clay min [%] | 16 Glt [%] | 17 Volc glass [%] | 18 Micronod [%] |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 0.03 | 70-507C-1-1,3 | 0 | 0 | 0 | SILICEOUS NANNOFOSSIL OOZE | relative abundance | 0 | 50 | 10 | 10 | 20 | 2 | 2 | 5 | 0 | 1 | 5 |
| 0.72 | 70-507C-1-1,72 | 0 | 0 | 0 | SILICEOUS FORAM-NANNO OOZE | relative abundance | 0 | 50 | 15 | 7 | 20 | 2 | 3 | 5 | 0 | 2 | 0 |
| 1.62 | 70-507C-1-2,12 | 0 | 0 | 0 | SILICEOUS FORAM NANNO OOZE | relative abundance | 5 | 40 | 30 | 5 | 10 | 2 | 3 | 5 | 0 | 1 | 0 |
| 3.08 | 70-507C-1-3,8 | 0 | 0 | 0 | SILICEOUS FORAM NANNO OOZE | relative abundance | 5 | 55 | 10 | 5 | 15 | 2 | 5 | 5 | 0 | 2 | 0 |
| 5.28 | 70-507C-1-4,78 | 0 | 0 | 0 | SILICEOUS FORAM NANNO OOZE | relative abundance | 5 | 50 | 20 | 5 | 10 | 2 | 3 | 5 | 0 | 2 | 0 |
| 6.73 | 70-507C-1-5,73 | 0 | 0 | 0 | relative abundance | 0 | 60 | 25 | 10 | 5 | 0 | 2 | 5 | 0 | 2 | 2 | |
| 8.18 | 70-507C-1-CC,0 | 0 | 0 | 0 | FORAMINIFERA NANNOFOSSIL OOZE | numerical abundance | 0 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 40 | 10 | 0 |