Benton, Laurie D; Ryan, Jeffrey; Tera, Fouad (2001): (Table 1) Boron abundance and isotopic ratios for ODP Site 125-779. PANGAEA, https://doi.org/10.1594/PANGAEA.711024, In supplement to: Benton, LD et al. (2001): Boron isotope systematics of slab fluids as inferred from a serpentine seamount, Mariana forearc. Earth and Planetary Science Letters, 187(3-4), 273-282, https://doi.org/10.1016/S0012-821X(01)00286-2
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: 19.512500 * Longitude: 146.696000
Date/Time Start: 1989-02-27T23:30:00 * Date/Time End: 1989-03-04T03:00:00
Minimum DEPTH, sediment/rock: 1.18 m * Maximum DEPTH, sediment/rock: 305.85 m
Event(s):
125-779A * Latitude: 19.512500 * Longitude: 146.696000 * Date/Time Start: 1989-02-28T10:00:00 * Date/Time End: 1989-03-04T03:00:00 * Elevation: -3958.0 m * Penetration: 317.2 m * Recovery: 73.24 m * Location: North Pacific Ocean * Campaign: Leg125 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 37 cores; 317.2 m cored; 0 m drilled; 23.1 % recovery
125-779B * Latitude: 19.512500 * Longitude: 146.696000 * Date/Time Start: 1989-02-27T23:30:00 * Date/Time End: 1989-02-28T10:00:00 * Elevation: -3958.0 m * Penetration: 9 m * Recovery: 8.7 m * Location: North Pacific Ocean * Campaign: Leg125 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 1 core; 9 m cored; 0 m drilled; 96.7 % recovery
Comment:
B concentrations for samples of serpentine matrix were measured by isotope dilution mass spectrometry (IDMS) at the Department of Terrestrial Magnetism (DTM) (Washington, DC, USA) using the HF-mannitol method of digestion (Nakamura et al., 1992) and positive ion thermal ionization mass spectrometry of Cs2BO[+]2 (Spivack and Edmond, 1986, doi:10.1021/ac00292a010, Xiao et al., 1988, doi:10.1016/0168-1176(88)83016-7). Concentrations for the clast samples were measured by direct-current plasma emission spectrometry (DCP) at the University of South Florida (Tampa, FL, USA) using the Na2CO3 flux method of digestion (Ryan and Langmuir, 1993, doi:10.1016/0016-7037(93)90008-K). Uncertainties are less than +/- 1% for IDMS measurements and +/- 10% for DCP measurements. B isotope measurements were prepared and analyzed using methods similar to the IDMS analyses at DTM.
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Event label | Event | ||||
2 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
3 | Sample code/label | Sample label | Benton, Laurie D | DSDP/ODP/IODP sample designation | ||
4 | Lithology/composition/facies | Lithology | Benton, Laurie D | |||
5 | δ11B | δ11B | ‰ SRM | Benton, Laurie D | Isotope ratio mass spectrometry | |
6 | δ11B, standard deviation | δ11B std dev | ± | Benton, Laurie D | Isotope ratio mass spectrometry | 2 sigma |
7 | Boron | B | mg/kg | Benton, Laurie D | Isotope ratio mass spectrometry |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
74 data points