Rare earth element abundances in hydrothermal fluids from the Manus Basin, Papua New Guinea: Indicators of sub-seafloor hydrothermal processes in back-arc basins-Reference-Cited by-同舟云学术

Rare earth element abundances in hydrothermal fluids from the Manus Basin, Papua New Guinea: Indicators of sub-seafloor hydrothermal processes in back-arc basins

Published:2010-10 Issue:19 Volume:74 Page:5494-5513
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Craddock Paul R.,Bach Wolfgang,Seewald Jeffrey S.,Rouxel Olivier J.,Reeves Eoghan,Tivey Margaret K.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference72 articles.

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3. Controls of fluid chemistry and complexation on rare-earth element contents of anhydrite from the Pacmanus subseafloor hydrothermal system, Manus Basin, Papua New Guinea;Bach;Miner. Deposita,2003

4. Variable basement composition and magma degassing affecting hydrothermal systems in the Eastern Manus Basin;Bach;EOS Trans. AGU. Fall Meet. Suppl.,2007

5. Rare-earth element mobility during hydrothermal and metamorphic fluid–rock interaction and the significance of the oxidation state of europium;Bau;Chem. Geol.,1991

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