Evidence for hydrothermal venting in Fe isotope compositions of the deep Pacific Ocean through time

Earth and Planetary Science Letters

Volumn 245, Issue 1-2, 2006, Pages 202-217

  Chu, N C ^a   Johnson, C M ^b   Beard, B L ^b   German, C R ^a   Nesbitt, R W ^a   Frank, M ^c   Bohn, Marcel ^d   Kubik, P W ^c   Usui, A ^e   Graham, I ^f  

^a NATIONAL OCEANOGRAPHY CENTRE   (United Kingdom)

^b UNIVERSITY OF WISCONSIN MADISON   (United States)

^c ETH ZURICH   (Switzerland)

^d CNRS   (France)

^e KOCHI UNIVERSITY   (Japan)

^f GNS SCIENCE   (New Zealand)

Author keywords

Fe isotopes; ferromanganese crusts; hydrothermal; Izu Bonin; Pacific Ocean

Indexed keywords

FERROMANGANESE CRUSTS; IRON ISOTOPES; ISOTOPE COMPOSITIONS; PACIFIC OCEAN;

COMPOSITION; CORRELATION METHODS; GEOCHEMISTRY; HYDROTHERMAL SYNTHESIS; IRON; ISOTOPES; SURFACE WATERS;

OCEANOGRAPHY;

FERROMANGANESE DEPOSIT; HYDROTHERMAL VENT; IRON; TEMPORAL VARIATION;

IZU-BONIN ARC; PACIFIC OCEAN;

EID: 33646060702     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2006.02.043     Document Type: Article

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