Davies, Thomas A; Luyendyk, Bruce P (2004): Mineral composition of silt fraction from Hole 26-250A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.220143
Always quote citation above when using data! You can download the citation in several formats below.
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:
X-ray mineralogy data base - Background and methods. hdl:10013/epic.32358.d001
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, silt fraction | ||
6 | Clinoptilolite | Cpt | % | X-ray diffraction, silt fraction | ||
7 | Cristobalite | Crs | % | X-ray diffraction, silt fraction | ||
8 | Gibbsite | Gbs | % | X-ray diffraction, silt fraction | ||
9 | Kaolinite | Kln | % | X-ray diffraction, silt fraction | ||
10 | Kalifeldspar | Kfs | % | X-ray diffraction, silt fraction | ||
11 | Mica | Mica | % | X-ray diffraction, silt fraction | ||
12 | Montmorillonite | Mnt | % | X-ray diffraction, silt fraction | ||
13 | Palygorskite | Plg | % | X-ray diffraction, silt fraction | ||
14 | Plagioclase | Pl | % | X-ray diffraction, silt fraction | ||
15 | Pyrite, FeS2 | Py | % | X-ray diffraction, silt fraction | ||
16 | Quartz | Qz | % | X-ray diffraction, silt fraction | ||
17 | Tridymite | Trd | % | X-ray diffraction, silt fraction |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
199 data points
Data
1 Depth sed [m] | 2 Sample label | 3 Depth top [m] | 4 Depth bot [m] | 5 Chl [%] | 6 Cpt [%] | 7 Crs [%] | 8 Gbs [%] | 9 Kln [%] | 10 Kfs [%] | 11 Mica [%] | 12 Mnt [%] | 13 Plg [%] | 14 Pl [%] | 15 Py [%] | 16 Qz [%] | 17 Trd [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
55.400 | 26-250A-1 | 54.5 | 56.30 | 0.6 | 9.9 | 12.2 | 22.6 | 17.7 | 37.0 | |||||||
56.150 | 26-250A-1 | 54.5 | 57.80 | 1.3 | 1.3 | 9.1 | 12.9 | 26.1 | 16.5 | 32.8 | ||||||
77.850 | 26-250A-3 | 73.5 | 82.20 | 0.7 | 16.7 | 15.5 | 21.0 | 14.7 | 1.6 | 29.7 | ||||||
114.450 | 26-250A-4 | 111.5 | 117.40 | 0.7 | 0.6 | 11.4 | 14.0 | 22.6 | 15.6 | 0.9 | 34.2 | |||||
189.450 | 26-250A-6 | 187.5 | 191.40 | 1.4 | 2.8 | 12.7 | 25.9 | 22.3 | 34.8 | |||||||
235.050 | 26-250A-7 | 235.0 | 235.10 | 1.2 | 4.6 | 13.0 | 27.3 | 18.4 | 1.3 | 34.2 | ||||||
238.500 | 26-250A-7 | 235.0 | 242.00 | 0.7 | 6.9 | 14.7 | 26.4 | 17.2 | 34.1 | |||||||
292.150 | 26-250A-8 | 292.0 | 292.30 | 1.4 | 4.8 | 13.4 | 24.4 | 18.3 | 37.7 | |||||||
350.450 | 26-250A-9 | 349.0 | 351.90 | 1.2 | 4.0 | 13.4 | 25.1 | 18.1 | 38.2 | |||||||
406.800 | 26-250A-10 | 406.0 | 407.60 | 1.1 | 1.5 | 12.6 | 23.8 | 18.3 | 42.7 | |||||||
463.150 | 26-250A-11 | 463.0 | 463.30 | 1.3 | 10.8 | 22.8 | 19.2 | 45.8 | ||||||||
466.600 | 26-250A-11 | 463.0 | 470.20 | 0.8 | 1.0 | 11.0 | 17.5 | 20.5 | 49.1 | |||||||
567.900 | 26-250A-13 | 567.5 | 568.30 | 0.6 | 0.6 | 13.7 | 15.6 | 21.2 | 48.3 | |||||||
568.150 | 26-250A-13 | 567.5 | 568.80 | 1.2 | 11.3 | 13.4 | 23.5 | 50.5 | ||||||||
606.350 | 26-250A-14 | 605.5 | 607.20 | 0.9 | 0.8 | 14.6 | 14.9 | 16.7 | 52.1 | |||||||
625.700 | 26-250A-15 | 624.5 | 626.90 | 2.5 | 22.7 | 22.5 | 17.2 | 35.2 | ||||||||
644.800 | 26-250A-17 | 643.5 | 646.10 | 1.0 | 2.8 | 13.9 | 20.4 | 19.7 | 42.1 | |||||||
663.400 | 26-250A-19 | 662.5 | 664.30 | 2.4 | 19.9 | 19.3 | 20.8 | 37.6 | ||||||||
682.750 | 26-250A-21 | 681.5 | 684.00 | 1.8 | 13.1 | 15.1 | 6.6 | 17.8 | 45.6 | |||||||
701.000 | 26-250A-23 | 700.5 | 701.50 | 72.2 | 1.7 | 1.3 | 4.5 | 2.3 | 4.7 | 13.3 | ||||||
711.400 | 26-250A-24 | 710.0 | 712.80 | 10.3 | 9.2 | 24.8 | 9.8 | 14.6 | 31.4 | |||||||
719.600 | 26-250A-25 | 719.5 | 719.70 | 3.0 | 20.1 | 28.0 | 15.8 | 33.2 |