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Pierre, Catherine; Rouchy, Jean Marie; Gaudichet, Annie (2000): (Table 1) Mineralogy and stable isotopic composition of diagenic carbonates from ODP Leg 164 sites [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.803853, In supplement to: Pierre, C et al. (2000): Diagenesis in the gas hydrate sediments of the Blake Ridge: mineralogy and stable isotope compositions of the carbonate and sulfide minerals. In: Paull, CK; Matsumoto, R; Wallace, PJ; Dillon, WP (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 164, 1-8, https://doi.org/10.2973/odp.proc.sr.164.226.2000

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Project(s):
Coverage:
Median Latitude: 32.313971 * Median Longitude: -75.678029 * South-bound Latitude: 31.785700 * West-bound Longitude: -75.930000 * North-bound Latitude: 32.983600 * East-bound Longitude: -75.468500
Date/Time Start: 1995-11-05T12:22:00 * Date/Time End: 1995-12-17T07:25:00
Minimum DEPTH, sediment/rock: 4.87 m * Maximum DEPTH, sediment/rock: 734.43 m
Event(s):
164-991A * Latitude: 32.983600 * Longitude: -75.930000 * Date/Time Start: 1995-11-05T12:22:00 * Date/Time End: 1995-11-05T14:18:00 * Elevation: -2567.5 m * Penetration: 56.6 m * Recovery: 58.56 m * Location: South Atlantic Ocean * Campaign: Leg164 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 6 cores; 56.6 m cored; 0 m drilled; 103.5 % recovery
164-992A * Latitude: 32.975700 * Longitude: -75.916000 * Date/Time Start: 1995-11-05T23:30:00 * Date/Time End: 1995-11-06T06:40:00 * Elevation: -2586.9 m * Penetration: 50.3 m * Recovery: 52.62 m * Location: South Atlantic Ocean * Campaign: Leg164 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 6 cores; 50.3 m cored; 0 m drilled; 104.6 % recovery
164-993A * Latitude: 32.962900 * Longitude: -75.894800 * Date/Time Start: 1995-11-06T08:49:00 * Date/Time End: 1995-11-07T06:15:00 * Elevation: -2641.8 m * Penetration: 51.9 m * Recovery: 45.7 m * Location: South Atlantic Ocean * Campaign: Leg164 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 6 cores; 51.9 m cored; 0 m drilled; 88.1 % recovery
Comment:
Sediment depth is given in mbsf. In situ temperatures have been deduced from the downhole measurements (Paull, Matsumoto, Wallace, et al., 1996, doi:10.2973/odp.proc.ir.164.1996). The d18O values of dolomite and siderite have been corrected for the differential phosphoric acid fractionation (Sharma and Clayton, 1965, doi:10.1016/0016-7037(65)90011-6; Carothers et al., 1988, doi:10.1016/0016-7037(88)90302-X). The d18O values of the diagenetic waters in equilibrium with the diagenetic dolomite, siderite, and calcite have been deduced from the 18O values of the carbonates and from the alpha values calculated for the in situ temperatures.
Size:
305 data points

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