Fluids in the peridotite–water system up to 6 GPa and 800°C: new experimental constrains on dehydration reactions
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/content/pdf/10.1007/s00410-010-0567-2.pdf
Reference48 articles.
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3. Ayers J, Dittmer SK, Layne GD (1997) Partitioning of elements between peridotite and H2O at 2.0–3.0 GPa and 900–1100 degrees C, and application to models of subduction zone processes. Earth Sci Planet Lett 150:381–398
4. Bose K, Ganguly J (1995) Quartz-coesite transition revisited: reversed experimental determination at 500–1200°C and retrieved thermochemical properties. Am Mineral 80:231–238
5. Brenan JM, Shaw HF, Ryerson FJ, Phinney DL (1995) Mineral-aqueous fluid partitioning of trace elements at 900°C and 2.0 GPa: Constraints on the trace element chemistry and deep crustal fluids. Geochim Cosmochim Acta 59:3331–3350
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