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Davies, Thomas A; Luyendyk, Bruce P (2004): Mineral composition of clay fraction from Hole 26-257. PANGAEA,

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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,
DSDP (1989): Data from the Deep Sea Drilling Project. Sediment, hard rock and reference files. National Geophysical Data Center, National Environmental Satellite, Data and Information Service, National Oceanic and Atmospheric Administration, U.S. Department of Commerce, 1, CD-ROM
Latitude: -30.986000 * Longitude: 108.349800
Date/Time Start: 1972-10-20T00:00:00 * Date/Time End: 1972-10-20T00:00:00
Minimum DEPTH, sediment/rock: 3.450 m * Maximum DEPTH, sediment/rock: 248.250 m
26-257 * Latitude: -30.986000 * Longitude: 108.349800 * Date/Time: 1972-10-20T00:00:00 * Elevation: -5278.0 m * Penetration: 326.5 m * Recovery: 77.1 m * Location: Indian Ocean//BASIN * Campaign: Leg26 * Basis: Glomar Challenger * Device: Drilling/drill rig (DRILL) * Comment: 16 cores; 146 m cored; 0 m drilled; 52.8 % recovery
#NameShort NameUnitPrincipal InvestigatorMethodComment
1DEPTH, sediment/rockDepthmGeocode
2Sample code/labelSample labelODP sample designation
3Depth, top/minDepth topm
4Depth, bottom/maxDepth botm
5ClinoptiloliteCpt%X-ray diffraction, clay fraction
6CristobaliteCrs%X-ray diffraction, clay fraction
7HaliteHl%X-ray diffraction, clay fraction
8Hematite, Fe2O3Hem%X-ray diffraction, clay fraction
9KaoliniteKln%X-ray diffraction, clay fraction
10KalifeldsparKfs%X-ray diffraction, clay fraction
11MicaMica%X-ray diffraction, clay fraction
12MontmorilloniteMnt%X-ray diffraction, clay fraction
13PlagioclasePl%X-ray diffraction, clay fraction
14QuartzQz%X-ray diffraction, clay fraction
15TridymiteTrd%X-ray diffraction, clay fraction
82 data points

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