Heinemann, Christiane; Füchtbauer, Hans (1982): (Table 3) Clay minerals in DSDP Leg 67 Holes [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.817248, In supplement to: Heinemann, C; Füchtbauer, H (1982): Insoluble residues of the fine-grained sediments from the trench transect south of Guatemala, Deep Sea Drilling Project Leg 67. In: Abouin, J; von Huene, R; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 67, 497-506, https://doi.org/10.2973/dsdp.proc.67.117.1982
Always quote citation above when using data! You can download the citation in several formats below.
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Median Latitude: 12.717743 * Median Longitude: -90.932786 * South-bound Latitude: 12.496300 * West-bound Longitude: -91.037700 * North-bound Latitude: 13.063700 * East-bound Longitude: -90.795200
Date/Time Start: 1979-05-17T00:00:00 * Date/Time End: 1979-06-18T00:00:00
Minimum DEPTH, sediment/rock: 2.90 m * Maximum DEPTH, sediment/rock: 428.50 m
Event(s):
67-494 * Latitude: 12.716700 * Longitude: -90.932800 * Date/Time: 1979-05-17T00:00:00 * Elevation: -5472.0 m * Penetration: 37.5 m * Recovery: 31.3 m * Location: North Pacific/TRENCH * Campaign: Leg67 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 4 cores; 37.5 m cored; 0 m drilled; 83.5 % recovery
67-494A * Latitude: 12.716800 * Longitude: -90.932800 * Date/Time: 1979-05-17T00:00:00 * Elevation: -5472.0 m * Penetration: 366.5 m * Recovery: 91.3 m * Location: North Pacific/TRENCH * Campaign: Leg67 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 35 cores; 329 m cored; 0 m drilled; 27.8 % recovery
67-495 * Latitude: 12.496300 * Longitude: -91.037700 * Date/Time: 1979-05-26T00:00:00 * Elevation: -4140.0 m * Penetration: 455.5 m * Recovery: 333.7 m * Location: North Pacific/TRENCH * Campaign: Leg67 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 48 cores; 446 m cored; 9.5 m drilled; 74.8 % recovery
Comment:
<1 indicate that very small percentages were detected. Samples in which kaolinite was identified by destruction of the X-ray peak upon heating to 500°C; partial destruction was interpreted by the presence of both kaolinite and chlorite; chlorite is listed if the peak did not change upon heating. Sediment depth is given in mbsf.
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Sample code/label | Sample label | Heinemann, Christiane | DSDP/ODP/IODP sample designation | ||
| 3 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 4 | Mixed layer clay minerals position | Mix layer | Å | Heinemann, Christiane | Polarisation microscopy | Swelling minerals, original |
| 5 | Mixed layer clay minerals position | Mix layer | Å | Heinemann, Christiane | Polarisation microscopy | Swelling minerals, glycolated |
| 6 | Smectite | Sme | % | Heinemann, Christiane | Polarisation microscopy | Clay minerals |
| 7 | Illite | Ill | % | Heinemann, Christiane | Polarisation microscopy | Clay minerals |
| 8 | Kaolinite | Kln | % | Heinemann, Christiane | Polarisation microscopy | Clay minerals |
| 9 | Kaolinite+Chlorite | Kln+Chl | % | Heinemann, Christiane | Polarisation microscopy | Clay minerals |
| 10 | Chlorite | Chl | % | Heinemann, Christiane | Polarisation microscopy | Clay minerals |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
512 data points