Davies, Thomas A; Luyendyk, Bruce P (2004): Mineral composition of clay fraction from Hole 26-250A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.219847
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Related to:
Doyle, Patricia S; Boltovskoy, Esteban; Herb, Rene C; Thierstein, Hans R; Hyndman, Roy D; Horvath, George J; Leidy, Rosanne D; McKelvey, Barrie C; Kempe, D R C; Rodolfo, Kelvin S; Davies, Thomas A; Luyendyk, Bruce P (1974): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XXVI, 1129 pp, https://doi.org/10.2973/dsdp.proc.26.1974
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: -33.462300 * Longitude: 39.369200
Date/Time Start: 1972-09-08T00:00:00 * Date/Time End: 1972-09-08T00:00:00
Minimum DEPTH, sediment/rock: 55.400 m * Maximum DEPTH, sediment/rock: 719.600 m
Event(s):
26-250A * Latitude: -33.462300 * Longitude: 39.369200 * Date/Time: 1972-09-08T00:00:00 * Elevation: -5119.0 m * Penetration: 737.5 m * Recovery: 124.2 m * Location: Indian Ocean//BASIN * Campaign: Leg26 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 26 cores; 238.5 m cored; 0 m drilled; 52.1 % 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 | Cristobalite | Crs | % | X-ray diffraction, clay fraction | ||
7 | Gibbsite | Gbs | % | X-ray diffraction, clay fraction | ||
8 | Halite | Hl | % | X-ray diffraction, clay fraction | ||
9 | Kaolinite | Kln | % | X-ray diffraction, clay fraction | ||
10 | Kalifeldspar | Kfs | % | X-ray diffraction, clay fraction | ||
11 | Mica | Mica | % | X-ray diffraction, clay fraction | ||
12 | Montmorillonite | Mnt | % | X-ray diffraction, clay fraction | ||
13 | Palygorskite | Plg | % | X-ray diffraction, clay fraction | ||
14 | Plagioclase | Pl | % | X-ray diffraction, clay fraction | ||
15 | Quartz | Qz | % | X-ray diffraction, clay fraction | ||
16 | Tridymite | Trd | % | X-ray diffraction, clay fraction |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
210 data points
Data
1 Depth sed [m] | 2 Sample label | 3 Depth top [m] | 4 Depth bot [m] | 5 Chl [%] | 6 Crs [%] | 7 Gbs [%] | 8 Hl [%] | 9 Kln [%] | 10 Kfs [%] | 11 Mica [%] | 12 Mnt [%] | 13 Plg [%] | 14 Pl [%] | 15 Qz [%] | 16 Trd [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
55.400 | 26-250A-1 | 54.5 | 56.30 | 0.8 | 13.5 | 5.0 | 15.1 | 45.7 | 3.5 | 16.2 | |||||
56.150 | 26-250A-1 | 54.5 | 57.80 | 13.1 | 6.0 | 14.4 | 36.7 | 7.4 | 4.7 | 17.7 | |||||
77.850 | 26-250A-3 | 73.5 | 82.20 | 13.2 | 3.3 | 11.5 | 55.7 | 3.8 | 12.5 | ||||||
114.450 | 26-250A-4 | 111.5 | 117.40 | 3.1 | 13.0 | 3.7 | 12.2 | 48.0 | 5.4 | 14.6 | |||||
189.450 | 26-250A-6 | 187.5 | 191.40 | 5.9 | 8.2 | 6.6 | 17.6 | 38.8 | 7.2 | 15.7 | |||||
235.050 | 26-250A-7 | 235.0 | 235.10 | 7.3 | 10.9 | 7.1 | 29.5 | 25.4 | 4.7 | 15.2 | |||||
238.500 | 26-250A-7 | 235.0 | 242.00 | 13.2 | 4.3 | 18.7 | 45.7 | 2.8 | 15.3 | ||||||
292.150 | 26-250A-8 | 292.0 | 292.30 | 1.7 | 10.7 | 6.2 | 20.0 | 43.6 | 2.7 | 15.1 | |||||
350.450 | 26-250A-9 | 349.0 | 351.90 | 3.9 | 10.1 | 7.9 | 23.9 | 29.3 | 7.4 | 17.5 | |||||
406.800 | 26-250A-10 | 406.0 | 407.60 | 3.5 | 7.1 | 7.4 | 37.0 | 24.4 | 4.1 | 16.5 | |||||
463.150 | 26-250A-11 | 463.0 | 463.30 | 2.1 | 7.6 | 5.9 | 24.6 | 34.1 | 5.3 | 20.4 | |||||
466.600 | 26-250A-11 | 463.0 | 470.20 | 5.2 | 7.3 | 5.8 | 24.9 | 31.7 | 4.2 | 20.9 | |||||
567.900 | 26-250A-13 | 567.5 | 568.30 | 2.2 | 9.2 | 2.6 | 5.8 | 25.2 | 31.2 | 4.7 | 19.1 | ||||
568.150 | 26-250A-13 | 567.5 | 568.80 | 7.8 | 6.4 | 5.1 | 27.2 | 19.2 | 6.4 | 27.8 | |||||
606.350 | 26-250A-14 | 605.5 | 607.20 | 3.1 | 7.1 | 8.0 | 22.5 | 33.6 | 3.1 | 22.6 | |||||
625.700 | 26-250A-15 | 624.5 | 626.90 | 9.4 | 8.4 | 6.5 | 22.5 | 41.7 | 11.5 | ||||||
644.800 | 26-250A-17 | 643.5 | 646.10 | 7.7 | 5.5 | 20.0 | 28.5 | 17.1 | 4.3 | 16.9 | |||||
663.400 | 26-250A-19 | 662.5 | 664.30 | 0.8 | 2.3 | 5.7 | 23.5 | 33.2 | 22.7 | 2.4 | 9.5 | ||||
682.750 | 26-250A-21 | 681.5 | 684.00 | 12.8 | 36.2 | 33.0 | 18.0 | ||||||||
701.000 | 26-250A-23 | 700.5 | 701.50 | 73.4 | 1.7 | 5.7 | 5.1 | 1.5 | 12.6 | ||||||
711.400 | 26-250A-24 | 710.0 | 712.80 | 8.0 | 52.9 | 29.8 | 9.4 | ||||||||
719.600 | 26-250A-25 | 719.5 | 719.70 | 2.5 | 9.5 | 50.6 | 29.0 | 8.5 |