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Teagle, Damon A H; Alt, Jeffrey C; Halliday, Alex N (1998): (Table 1) Strontium concentrations and isotope ratios of anhydrite from DSDP/ODP Hole 504B [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.711801, In supplement to: Teagle, DAH et al. (1998): Tracing the chemical evolution of fluids during hydrothermal recharge: Constraints from anhydrite recovered in ODP Hole 504B. Earth and Planetary Science Letters, 155(3-4), 167-182, https://doi.org/10.1016/S0012-821X(97)00209-4

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Abstract:
In samples from 1575 to 1982 mbsf anhydrite leached from whole-rock powders. 87Sr/86Sr and Sr/Ca determined following methods described in (Teagle et al., 1996, doi:10.2973/odp.proc.sr.148.113.1996, Teagle et al., 1998, doi:10.2973/odp.proc.sr.158.223.1998). For the period of the analysis (Jan. 1994-Dec. 1995) NIST SRM 987 gave 87Sr/86Srs0.710244 +/- 0.000018 (2 sigma, n = 115). Full analytical procedural blanks were <50 pg for Sr. delta18O following (Pickthorn and O´Neil, 1985). Repeated extractions and measurements of samples and standards were reproducible within +/- 0.5.
Coverage:
Median Latitude: 1.226980 * Median Longitude: -83.730220 * South-bound Latitude: 1.226900 * West-bound Longitude: -83.730300 * North-bound Latitude: 1.227200 * East-bound Longitude: -83.730000
Date/Time Start: 1979-12-04T00:00:00 * Date/Time End: 1991-11-12T04:10:00
Minimum DEPTH, sediment/rock: 580 m * Maximum DEPTH, sediment/rock: 1982 m
Event(s):
70-504B * Latitude: 1.227000 * Longitude: -83.730000 * Date/Time: 1979-12-04T00:00:00 * Elevation: -3460.0 m * Penetration: 836.1 m * Recovery: 91.6 m * Campaign: Leg70 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 40 cores; 328.6 m cored; 18.5 m drilled; 27.9 % recovery
83-504B * Latitude: 1.227200 * Longitude: -83.730200 * Date/Time Start: 1981-11-22T00:00:00 * Date/Time End: 1982-01-02T00:00:00 * Elevation: -3460.0 m * Penetration: 1350 m * Recovery: 107.7 m * Campaign: Leg83 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: Leg 83 of DSDP was devoted entirely to coring and experiments in Hole 504B, the deepest borehole to date into the oceanic crust. Hole 504B now extends over a kilometer into basement, nearly twice as far as any other DSDP hole, and it is the only DSDP hole to have clearly penetrated into the intrusive sheeted dikes that underlie the extrusive pillow lavas of the upper oceanic crust. At Hole 504B, Leg 83 continued an ongoing DSDP effort that began during Legs 68, 69, and 70 in 1979, and also included part of Leg 92 in 1983. 71 cores; 514 m cored; 0 m drilled; 21 % recovery
111-504B * Latitude: 1.226900 * Longitude: -83.730300 * Date/Time Start: 1986-10-05T11:45:00 * Date/Time End: 1986-10-16T18:15:00 * Elevation: -3474.0 m * Penetration: 1562.1 m * Recovery: 27.36 m * Location: North Pacific Ocean * Campaign: Leg111 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 29 cores; 209 m cored; 0 m drilled; 13.1 % recovery
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEvent
2DEPTH, sediment/rockDepth sedmGeocode
3Sample code/labelSample labelTeagle, Damon A HDSDP/ODP/IODP sample designation
4Sample code/label 2Sample label 2Teagle, Damon A Hpiece no
5Strontium-87/Strontium-86 ratio87Sr/86SrTeagle, Damon A HIsotope ratio mass spectrometry
6Strontium-87/Strontium-86 ratio, error87Sr/86Sr e±Teagle, Damon A HIsotope ratio mass spectrometry
7--Teagle, Damon A HX-MORB is the proportion of MORB-derived Sr in anhydrite compared to 6-Ma-old and modern seawater for (87Sr/86Sr)MORB = 0.7025, (87Sr/86Sr)6 Ma-SW = 0.70896 and (87Sr/86Sr)modern-SW = 0.70918
8Strontium/Calcium ratioSr/CaTeagle, Damon A Hmmol/mol
9StrontiumSrmg/kgTeagle, Damon A H
10δ18Oδ18OTeagle, Damon A HIsotope ratio mass spectrometrySMOW
11Temperature, calculatedT cal°CTeagle, Damon A HCalculatedof formation calculated from the fractionation equation (Chiba et al., 1985, doi:10.1016/0012-821X(81)90025-X) for 0 seawater
12δ34Sδ34S‰ CDTTeagle, Damon A HIsotope ratio mass spectrometry
Size:
162 data points

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