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Lackschewitz, Klas Sven; Devey, Colin W; Stoffers, Peter; Botz, Reiner; Eisenhauer, Anton; Kummetz, M; Schmidt, Mark; Singer, A (2004): (Table 2) Mineralogical assemblages of the clay fraction (<2 µm) of altered felsic rocks from ODP Hole 193-1189A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.710736, In supplement to: Lackschewitz, KS et al. (2004): Mineralogical, geochemical and isotopic characteristics of hydrothermal alteration processes in the active, submarine, felsic-hosted PACMANUS field, Manus Basin, Papua New Guinea. Geochimica et Cosmochimica Acta, 68(21), 4405-4427, https://doi.org/10.1016/j.gca.2004.04.016

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Project(s):
Coverage:
Latitude: -3.720700 * Longitude: 151.674900
Date/Time Start: 2000-11-22T08:30:00 * Date/Time End: 2000-11-23T20:45:00
Minimum DEPTH, sediment/rock: 10.92 m * Maximum DEPTH, sediment/rock: 116.33 m
Event(s):
193-1189A * Latitude: -3.720700 * Longitude: 151.674900 * Date/Time Start: 2000-11-22T08:30:00 * Date/Time End: 2000-11-23T20:45:00 * Elevation: -1690.2 m * Penetration: 125.8 m * Recovery: 8.58 m * Location: Bismarck Sea * Campaign: Leg193 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 13 cores; 125.8 m cored; 0 m drilled; 6.8 % recovery
Size:
50 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Depth sed [m]

Sample label
(DSDP/ODP/IODP sample designation)

Chl
(X-ray diffraction (XRD))

Minerals
(illite, X-ray diffraction (XRD))

Minerals
(cristobalite, X-ray diffracti...)

Minerals
(K-feldspar, X-ray diffraction...)

Min assembl
(chlorite-vermiculite mixed-la...)

Qz
(X-ray diffraction (XRD))

Pl
(X-ray diffraction (XRD))
10.92193-1189A-2R-1,122-12550-90%50-90%5-50%<2%
19.54193-1189A-3R-1,14-1750-90%5-50%<2%<2%2-5%
29.24193-1189A-4R-1,14-1750-90%2-5%<2%<2%
38.97193-1189A-5R-1,17-2050-90%5-50%<2%
58.60193-1189A-7R-1,30-3350-90%5-50%2-5%
77.70193-1189A-9R-1,0-550-90%2-5%2-5%5-50%
78.33193-1189A-9R-1,63-6750-90%5-50%<2%
88.07193-1189A-10R-1,77-8150-90%5-50%2-5%2-5%<2%
97.20193-1189A-11R-1,30-335-50%50-90%
107.33193-1189A-12R-1,83-8650-90%5-50%<2%
116.33193-1189A-13R-1,23-33>90%2-5%<2%