Maher, Katharine et al. (2004): Rates of silicate dissolution in deep-sea sediment; in situ measurement using (super 234) U/ (super 238) U of pore fluids

Leg/Site/Hole:
ODP 162
ODP 162 984
Identifier:
2005-026036
georefid

10.1016/j.gca.2004.04.024
doi

Creator:
Maher, Katharine
University of California, Department of Earth and Planetary Science, Berkeley, CA, United States
author

DePaolo, Donald J.
Lawrence Berkeley National Laboratory, United States
author

Lin, Jo Chiu-Fang
author

Identification:
Rates of silicate dissolution in deep-sea sediment; in situ measurement using (super 234) U/ (super 238) U of pore fluids
2004
Coverage:Geographic coordinates:
North:61.2532
West:-24.0457East: -24.0457
South:61.2532

Sedimentary petrology; Isotope geochemistry; actinides; Atlantic Ocean; Bjorn Drift; carbonates; chemical composition; clastic sediments; clay; deep-sea sedimentation; Europe; fluid phase; geochemistry; Iceland; Iceland-Faeroe Ridge; ICP mass spectra; in situ; isotope ratios; isotopes; Leg 162; liquid phase; marine sedimentation; marine sediments; mass spectra; mathematical methods; measurement; metals; mineral composition; models; North Atlantic; Ocean Drilling Program; ODP Site 984; pore water; radioactive isotopes; recrystallization; Reykjanes Ridge; Rockall Plateau; Rockall Trough; sedimentation; sedimentation rates; sediments; silicates; silt; solid phase; solution; spectra; thermal ionization mass spectra; U-238/U-234; uranium; weathering; Western Europe; Wyville-Thomson Ridge;

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