Oceanic molybdenum isotope fractionation: Diagenesis and hydrothermal ridge-flank alteration-Reference-Cited by-同舟云学术

Oceanic molybdenum isotope fractionation: Diagenesis and hydrothermal ridge-flank alteration

Published:2002-12 Issue:12 Volume:3 Page:1-9
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem.-Geophys.-Geosyst.

Author:

McManus James¹,Nägler Thomas F.²,Siebert Christopher²,Wheat C. Geoffrey³,Hammond Douglas E.⁴

Affiliation:

1. Large Lakes Observatory; University of Minnesota; Duluth Minnesota 55812 USA

2. Universitåt Bern; Institut für Geologie; CH-3012 Bern, Erlachstrasse 9a Switzerland

3. Global Undersea Research Unit; P.O. Box 475, Moss Landing California 95039 USA

4. University of Southern California; Department of Earth Sciences; Los Angeles California 90089 USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference54 articles.

1. Iron isotope biosignatures: Promise and progress (abstract);Anbar;Eos Trans. AGU,2001

2. Precise determination of Mass-dependent variations in the isotopic composition of molybdenum using MC-ICPMS;Anbar;Anal. Chem.,2001

3. Experimental study of mass-dependent fractionation of molybdenum isotopes scavenged during precipitation of manganese oxyhydroxides;Barling;Eos Trans. AGU,2001

4. Natural mass-dependent variations in the isotopic composition of molybdenum;Barling;Earth Planet. Sci. Lett.,2001

5. A geological and geophysical investigation of Baby Bare, locus of a ridge-flank hydrothermal system in the Cascadia Basin;Becker;J. Geophys. Res.,2000

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