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Gersonde, Rainer; Shipboard Scientific Party (2001): X-ray diffraction data for Site 177-1089. PANGAEA, https://doi.org/10.1594/PANGAEA.60149

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Related to:
Gersonde, Rainer; Hodell, David A; Blum, Peter; et al. (1999): Proceedings of the Ocean Drilling Program, 177 Initial Reports. Proceedings of the Ocean Drilling Program, Ocean Drilling Program, 177, online, https://doi.org/10.2973/odp.proc.ir.177.1999
Project(s):
Coverage:
Latitude: -40.936333 * Longitude: 9.893983
Date/Time Start: 1997-12-19T00:00:00 * Date/Time End: 1997-12-19T00:00:00
Minimum DEPTH, sediment/rock: 0.78 m * Maximum DEPTH, sediment/rock: 261.29 m
Event(s):
177-1089 * Latitude: -40.936333 * Longitude: 9.893983 * Date/Time: 1997-12-19T00:00:00 * Elevation: -4620.5 m * Penetration: 793.6 m * Recovery: 675.9 m * Location: South Atlantic Ocean * Campaign: Leg177 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 86 cores; 791.6 m cored; 2 m drilled; 85.4% recovery
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DEPTH, sediment/rockDepthmGeocode
2Depth, compositeDepth compmcdShipboard Scientific PartyIntercore correlation
3Sample code/labelSample labelShipboard Scientific PartyDSDP/ODP/IODP sample designation
4Calcium carbonateCaCO3%Shipboard Scientific PartyElement analysis coulometric
5Opal, carbonate free fractionSiO2 carb free%Shipboard Scientific PartyX-ray diffraction, calcaluted from intensity
6Opal, biogenic silicabSiO2%Shipboard Scientific PartyX-ray diffraction, calcaluted from intensity
7SiliciclasticsSiliciclast%Shipboard Scientific PartyX-ray diffraction (XRD)
8Pyrite, FeS2Py%Shipboard Scientific PartyX-ray diffraction, calculated from peak area
9Quartz/Feldspar ratioQz/FspShipboard Scientific PartyX-ray diffraction, calculated from peak area
10Clay minerals/feldspar+quartz ratioClay/Fsp+QzShipboard Scientific PartyX-ray diffraction, calculated from peak area
11Clay 10Å/7Å ratioClay 10Å/7ÅShipboard Scientific PartyX-ray diffraction, calcaluted from intensity
Size:
489 data points

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