The solubility of rocks in metamorphic fluids: A model for rock-dominated conditions to upper mantle pressure and temperature-Reference-Cited by-同舟云学术

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The solubility of rocks in metamorphic fluids: A model for rock-dominated conditions to upper mantle pressure and temperature

Published:2015-11 Issue: Volume:430 Page:486-498
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Galvez Matthieu E.,Manning Craig E.,Connolly James A.D.,Rumble Douglas

Funder

Carnegie Fellowship

NASA

National Science Foundation

Deep Carbon Observatory

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference80 articles.

1. Mass transfer during Barrovian metamorphism of pelites, south-central Connecticut; I, Evidence for changes in composition and volume;Ague;Am. J. Sci.,1994

2. Carbon dioxide released from subduction zones by fluid-mediated reactions;Ague;Nat. Geosci.,2014

3. Nitrogen-bearing, aqueous fluid inclusions in some eclogites from the Western Gneiss Region of the Norwegian Caledonides;Andersen;Contrib. Mineral. Petrol.,1989

4. Channelized fluid flow and eclogite-facies metasomatism along the subduction shear zone;Angiboust;J. Petrol.,2014

5. Experimental determination of CO2–H2O activity–composition relations at 600–1000 °C and 6–14 kbar by reversed decarbonation and dehydration reactions;Aranovich;Am. Mineral.,1999

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