Metamorphic reaction rate controlled by fluid pressure not confining pressure: implications of dehydration experiments with gypsum-Reference-Cited by-同舟云学术

Metamorphic reaction rate controlled by fluid pressure not confining pressure: implications of dehydration experiments with gypsum

Published:2012-02-21 Issue:1 Volume:164 Page:69-79
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contrib Mineral Petrol

Author:

Llana-Fúnez Sergio,Wheeler John,Faulkner D. R.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/s00410-012-0726-8.pdf

Reference39 articles.

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2. Bear J, Bachmat Y (1991) Introduction to modelling of transport phenomena in porous media. Kluwer, London

3. Bruton CJ, Helgeson HC (1983) Calculation of the chemical and thermodynamic consequences of differences between fluid and geostatic pressure in hydrothermal systems. Am J Sci 283A:540–588

4. Dahlen FA (1992) Metamorphism of nonhydrostatically stressed rocks. Am J Sci 292(3):184–198

5. de Meer S, Spiers CJ (1995) Creep of wet gypsum aggregates under hydrostatic loading conditions. Tectonophysics 245(3–4):171–183

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