Sulphide mineral evolution and metal mobility during alteration of the oceanic crust: Insights from ODP Hole 1256D-Reference-Cited by-同舟云学术

Sulphide mineral evolution and metal mobility during alteration of the oceanic crust: Insights from ODP Hole 1256D

Published:2016-11 Issue: Volume:193 Page:132-159
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Patten C.G.C.,Pitcairn I.K.,Teagle D.A.H.,Harris M.

Funder

Stockholm University

Swedish Research Council

NSF

Japan’s Ministry of Education, Culture, Sports, Science, and Technology

European Consortium for Ocean Research Drilling

Australia-New Zealand IODP Consortium

People’s Republic of China Ministry of Science and Technology

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

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3. Ion microprobe analyses of the sulfur isotopic composition of sulfides in hydrothermally altered rocks, DSDP/ODP Hole 504B1;Alt;Proc. Ocean Drill. Progr. Sci. Results,1989

4. Microbial sulfate reduction and the sulfur budget for a complete section of altered oceanic basalts, IODP Hole 1256D (eastern Pacific);Alt;Earth Planet. Sci. Lett.,2011

5. Hydrothermal alteration and fluid fluxes in ophiolites and oceanic crust;Alt;Spec. Papers Geol. Soc. Am.,2000

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