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Snyder, Glen T; Savov, Ivan P; Muramatsu, Yasuyuki (2005): (Table T1) Iodine and boron concentrations in interstitial waters of ODP Site 195-1200 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.778443, In supplement to: Snyder, GT et al. (2005): Iodine and boron in Mariana serpentinite mud volcanoes (ODP Legs 125 and 195): implications for forearc processes and subduction recycling. In: Shinohara, M; Salisbury, MH; Richter, C (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 195, 1-18, https://doi.org/10.2973/odp.proc.sr.195.102.2005

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Related to:
Snyder, Glen T; Fehn, Udo; Goff, F (2002): Iodine isotope ratios and halide concentrations in fluids of the Satsuma-Iwojima volcano, Japan. Earth Planets and Space, 54, 265-273, https://doi.org/10.1186/BF03353026
Project(s):
Coverage:
Median Latitude: 13.783705 * Median Longitude: 146.002975 * South-bound Latitude: 13.783350 * West-bound Longitude: 146.002850 * North-bound Latitude: 13.784060 * East-bound Longitude: 146.003100
Date/Time Start: 2001-03-26T05:00:00 * Date/Time End: 2001-03-28T11:15:00
Minimum DEPTH, sediment/rock: 1.20 m * Maximum DEPTH, sediment/rock: 56.02 m
Event(s):
195-1200D * Latitude: 13.784060 * Longitude: 146.002850 * Date/Time Start: 2001-03-26T05:00:00 * Date/Time End: 2001-03-27T12:30:00 * Elevation: -2931.0 m * Penetration: 44.4 m * Recovery: 22 m * Location: North Pacific Ocean * Campaign: Leg195 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 10 cores; 21.9 m cored; 22.5 m drilled; 100.5 % recovery
195-1200E * Latitude: 13.783350 * Longitude: 146.003100 * Date/Time Start: 2001-03-27T12:30:00 * Date/Time End: 2001-03-28T11:15:00 * Elevation: -2911.0 m * Penetration: 56.4 m * Recovery: 38.06 m * Location: North Pacific Ocean * Campaign: Leg195 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 10 cores; 54.4 m cored; 2 m drilled; 70 % recovery
Comment:
Sediment depth is given in mbsf. For representative concentrations of I, B and Cl for seawater see Broecker and Peng (1982, doi:10.1016/0016-7037(83)90075-3), for nonserpentinite mud volcano fluids see Aloisi et al. (2004, doi:10.1016/j.epsl.2004.07.006), for décollement fluids see You et al., (1993, doi:10.2973/odp.proc.sr.131.116.1993) and Kastner et al. (1993, doi:10.2973/odp.proc.sr.131.143.1993), and for high-temperature fumarolic condensate (885°C) see Snyder et al. (2002) and Goff and McMurtry (2000, doi:10.1016/S0377-0273(99)00177-8).
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEvent
2Sample code/labelSample labelSnyder, Glen TDSDP/ODP/IODP sample designation
3DEPTH, sediment/rockDepth sedmGeocode
4IodineIµmol/lSnyder, Glen TInductively coupled plasma - mass spectrometry (ICP-MS)
5BoronBµmol/lSnyder, Glen TInductively coupled plasma atomic emission spectroscope (ICP-AES)
6ChlorideCl-mmol/lSnyder, Glen Tfrom nearest corresponding pore fluid splits analyzed onboard (Salisbury et al., 2002, doi:10.2973/odp.proc.ir.195.2002)
7IodineIµmol/lSnyder, Glen TCalculatednormalized to the bulk wet sediment volume (mmol/m**3), calculated from measured concentrations (this study) and sediment porosity (Salisbury et al., 2002, doi:10.2973/odp.proc.ir.195.2002)
8BoronBµmol/lSnyder, Glen TCalculatednormalized to the bulk wet sediment volume (mmol/m**3), calculated from measured concentrations (this study) and sediment porosity (Salisbury et al., 2002, doi:10.2973/odp.proc.ir.195.2002)
Size:
66 data points

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