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Wright, James D; Miller, Kenneth G (1992): (Table 2) Stable oxygen isotope event stratigraphy and associated ages of ODP Hole 120-747A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.758915, In supplement to: Wright, JD; Miller, KG (1992): Miocene stable isotope stratigraphy, Site 747, Kerguelen Plateau. In: Wise, SW; Schlich, R; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 120, 855-866, https://doi.org/10.2973/odp.proc.sr.120.193.1992

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Project(s):
Coverage:
Latitude: -54.811000 * Longitude: 76.794000
Date/Time Start: 1988-03-06T22:30:00 * Date/Time End: 1988-03-08T17:15:00
Minimum DEPTH, sediment/rock: 37.40 m * Maximum DEPTH, sediment/rock: 117.50 m
Event(s):
120-747A * Latitude: -54.811000 * Longitude: 76.794000 * Date/Time Start: 1988-03-06T22:30:00 * Date/Time End: 1988-03-08T17:15:00 * Elevation: -1706.0 m * Penetration: 256 m * Recovery: 227.34 m * Location: South Indian Ridge, South Indian Ocean * Campaign: Leg120 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 27 cores; 256 m cored; 0 m drilled; 88.8 % recovery
Comment:
GPTS = Geomagnetic Polarity Time Scale from Berggren et al. (1985). Zone Mi7 is not formally recognized as an isotope chronozone, but it is useful in upper Miocene correlations (Wright et al., 1991).
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Datum levelDLWright, James DEvent
2ChronozoneChronozoneWright, James DGPTS correlation (after Berggren 1985)
3Age modelAge modelkaWright, James DEstimated ages are derived by d18O correlation of Sites 563 and 608 stable isotope events to the GPTS (Miller et al., 1991a), except for the ages indicated by #
4DEPTH, sediment/rockDepth sedmGeocode
5Age model, optionalAge model optkaWright, James DInitial age estimate
Size:
32 data points

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