Coupled molybdenum, iron and uranium stable isotopes as oceanic paleoredox proxies during the Paleoproterozoic Shunga Event

Chemical Geology

Volumn 362, Issue , 2013, Pages 193-210

  Asael, Dan ^a,b   Tissot, François L H ^c   Reinhard, Christopher T ^d,e   Rouxel, Olivier ^a   Dauphas, Nicolas ^c   Lyons, Timothy W ^e   Ponzevera, Emmanuel ^a   Liorzou, Céline ^b   Chéron, Sandrine ^a  

^a IFREMER   (France)

^b UNIVERSITÉ DE BRETAGNE OCCIDENTALE   (France)

^c UNIVERSITY OF CHICAGO   (United States)

^d CALIFORNIA INSTITUTE OF TECHNOLOGY   (United States)

^e UNIVERSITY OF CALIFORNIA   (United States)

Author keywords

Euxinic; Iron isotopes; Molybdenum isotopes; Paleoproterozoic; Shunga Event; Uranium isotopes

Indexed keywords

EUXINIC; IRON ISOTOPES; MOLYBDENUM ISOTOPES; PALEOPROTEROZOIC; SHUNGA EVENT; URANIUM ISOTOPES;

DESULFURIZATION; GALLIUM; MOLYBDENUM; NUCLEAR FUELS; OCEANOGRAPHY; OXYGEN; PYRITES; SHALE;

ISOTOPES;

CARBON ISOTOPE; CHEMOSTRATIGRAPHY; IRON; ISOTOPIC COMPOSITION; METAMORPHISM; MOLYBDENUM; OXIDATION; PROTEROZOIC; PYRITE; PYRRHOTITE; REDOX CONDITIONS; SPECIATION (CHEMISTRY); URANIUM ISOTOPE;

ARKHANGELSK [RUSSIAN FEDERATION]; ONEGA BASIN; RUSSIAN FEDERATION;

EID: 84889584059     PISSN: 00092541     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.chemgeo.2013.08.003     Document Type: Article

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