Oceanic molybdenum isotope fractionation: Diagenesis and hydrothermal ridge-flank alteration
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چکیده
منابع مشابه
Oceanic molybdenum isotope fractionation: Diagenesis and hydrothermal ridgeâ•’flank alteration
[1] Isotopic analyses of dissolved molybdenum are presented for sediment pore waters from a reducing sedimentary basin and for fluids from a low-temperature ridge flank hydrothermal system. dMo in these fluids range from 0.8 to 3.5% (relative to a laboratory standard), demonstrating that marine sedimentary reactions significantly fractionate Mo isotopes. Within the upper 3 cm of sediment, manga...
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ژورنال
عنوان ژورنال: Geochemistry, Geophysics, Geosystems
سال: 2002
ISSN: 1525-2027
DOI: 10.1029/2002gc000356