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Irino, Tomohisa; Tada, Ryuji (2000): (Table A2) Mineral composition and detritus content of ODP Hole 127-797B sediments. Geological Institute, University of Tokyo, PANGAEA, https://doi.org/10.1594/PANGAEA.726530, In supplement to: Irino, T; Tada, R (2000): Quantification of aeolian dust (Kosa) contribution to the Japan Sea sediments and its variation during the last 200 ky. Geochemical Journal, 34(1), 59-93, https://doi.org/10.2343/geochemj.34.59

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Project(s):
Coverage:
Latitude: 38.616000 * Longitude: 134.536000
Date/Time Start: 1989-07-31T20:00:00 * Date/Time End: 1989-08-04T17:00:00
Minimum DEPTH, sediment/rock: 0.13 m * Maximum DEPTH, sediment/rock: 12.99 m
Event(s):
127-797B * Latitude: 38.616000 * Longitude: 134.536000 * Date/Time Start: 1989-07-31T20:00:00 * Date/Time End: 1989-08-04T17:00:00 * Elevation: -2874.0 m * Penetration: 495.7 m * Recovery: 370.69 m * Location: Japan Sea * Campaign: Leg127 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 53 cores; 495.7 m cored; 0 m drilled; 74.8 % recovery
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Sample code/labelSample labelIrino, TomohisaDSDP/ODP/IODP sample designation
2DEPTH, sediment/rockDepthmGeocode
3SmectiteSme%Irino, TomohisaX-ray diffraction (MAC Science MXP-3)
4IlliteIll%Irino, TomohisaX-ray diffraction (MAC Science MXP-3)
5ChloriteChl%Irino, TomohisaX-ray diffraction (MAC Science MXP-3)
6AmphiboleAmp%Irino, TomohisaX-ray diffraction (MAC Science MXP-3)
7QuartzQz%Irino, TomohisaX-ray diffraction (MAC Science MXP-3)
8FeldsparFsp%Irino, TomohisaX-ray diffraction (MAC Science MXP-3)
9AmorphicsAmorphics%Irino, TomohisaCalculateddetrital amorphous material
10CalciteCal%Irino, TomohisaX-ray diffraction (MAC Science MXP-3)
11Pyrite, FeS2Py%Irino, TomohisaX-ray diffraction (MAC Science MXP-3)
12Manganese carbonate, rhodochrositeRds%Irino, TomohisaX-ray diffraction (MAC Science MXP-3)
13DetritusDetritus%Irino, TomohisaCalculated
14Sample commentSample commentIrino, Tomohisa
Size:
2412 data points

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