Burns, Robert E; Andrews, James E (2004): Mineral composition of clay fraction from Hole 21-206 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.219801
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Related to:
Burns, Robert E; Andrews, James E; van der Lingen, Gerrit J; Churkin, M; Galehouse, J S; Packham, G H; Davies, Thomas A; Kennett, James P; Dumitrica, Paulian (1973): Initial Reports of the Deep Sea Drilling Project,. U. S. Government Printing Office, XXI, 931 pp, https://doi.org/10.2973/dsdp.proc.21.1973
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: -32.012500 * Longitude: 165.452500
Date/Time Start: 1971-11-30T00:00:00 * Date/Time End: 1971-11-30T00:00:00
Minimum DEPTH, sediment/rock: 1.050 m * Maximum DEPTH, sediment/rock: 398.650 m
Event(s):
21-206 * Latitude: -32.012500 * Longitude: 165.452500 * Date/Time: 1971-11-30T00:00:00 * Elevation: -3196.0 m * Penetration: 416 m * Recovery: 243.5 m * Location: South Pacific/Tasman Sea/BASIN * Campaign: Leg21 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 45 cores; 400 m cored; 0 m drilled; 60.9 % 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 | Depth, top/min | Depth top | m | |||
4 | Depth, bottom/max | Depth bot | m | |||
5 | Chlorite | Chl | % | X-ray diffraction, clay fraction | ||
6 | Kaolinite | Kln | % | X-ray diffraction, clay fraction | ||
7 | Mica | Mica | % | X-ray diffraction, clay fraction | ||
8 | Montmorillonite | Mnt | % | X-ray diffraction, clay fraction | ||
9 | Plagioclase | Pl | % | X-ray diffraction, clay fraction | ||
10 | Quartz | Qz | % | X-ray diffraction, clay fraction |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
102 data points
Data
1 Depth sed [m] | 2 Sample label | 3 Depth top [m] | 4 Depth bot [m] | 5 Chl [%] | 6 Kln [%] | 7 Mica [%] | 8 Mnt [%] | 9 Pl [%] | 10 Qz [%] |
---|---|---|---|---|---|---|---|---|---|
1.050 | 21-206-1 | 0.0 | 2.10 | 25.7 | 34.6 | 8.7 | 31.0 | ||
81.150 | 21-206-10 | 80.0 | 82.30 | 3.8 | 9.8 | 36.9 | 16.5 | 10.7 | 22.3 |
117.300 | 21-206-14 | 116.0 | 118.60 | 1.6 | 17.3 | 14.2 | 39.2 | 7.0 | 20.7 |
127.050 | 21-206-15 | 125.0 | 129.10 | 1.9 | 19.2 | 21.3 | 29.1 | 7.4 | 21.2 |
154.800 | 21-206-18 | 152.0 | 157.60 | 1.4 | 16.7 | 20.3 | 36.6 | 5.5 | 19.6 |
175.050 | 21-206-20 | 174.0 | 176.10 | 22.6 | 34.9 | 12.3 | 30.2 | ||
194.000 | 21-206-22 | 192.0 | 196.00 | 10.6 | 14.9 | 56.1 | 5.5 | 12.8 | |
229.800 | 21-206-26 | 228.0 | 231.60 | 1.7 | 14.2 | 11.2 | 56.0 | 3.4 | 13.5 |
278.800 | 21-206-31 | 277.0 | 280.60 | 1.7 | 16.5 | 11.4 | 43.3 | 7.0 | 20.2 |
304.900 | 21-206-34 | 304.0 | 305.80 | 2.5 | 5.6 | 7.2 | 51.9 | 5.6 | 27.2 |
363.050 | 21-206-40 | 362.0 | 364.10 | 7.7 | 3.4 | 50.7 | 10.8 | 27.4 | |
398.650 | 21-206-44 | 398.0 | 399.30 | 1.6 | 2.4 | 3.5 | 26.2 | 6.9 | 59.4 |