Fluid-induced Dehydration of the Paleoarchean Sand River Biotite-Hornblende Gneiss, Central Zone, Limpopo Complex, South Africa-Reference-Cited by-同舟云学术

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Fluid-induced Dehydration of the Paleoarchean Sand River Biotite-Hornblende Gneiss, Central Zone, Limpopo Complex, South Africa

Published:2012-09-29 Issue:1 Volume:54 Page:41-74
ISSN:0022-3530
Container-title:Journal of Petrology
language:en
Short-container-title:Journal of Petrology

Author:

Rajesh H. M.,Belyanin G. A.,Safonov O. G.,Kovaleva E. I.,Golunova M. A.,Van Reenen D. D.

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Link

http://academic.oup.com/petrology/article-pdf/54/1/41/4243177/egs062.pdf

Reference105 articles.

1. H 2 O activity in concentrated NaCl solutions at high pressures and temperatures measured by the brucite-periclase equilibrium

2. H 2 O activity in concentrated KCl and KCl-NaCl solutions at high temperatures and pressures measured by the brucite-periclase equilibrium

3. Reversed determination of the reaction; phlogopite+quartz = enstatite+potassium feldspar+H2O in the ranges 750-875 degrees C and 2-12 kbar at low H2O activity with concentrated KCl solutions

4. THE H2O AND CO2 REGIME IN REGIONAL METAMORPHISM

5. The Messina Layered Intrusion, Limpopo Belt, South Africa: An example of in-situ contamination of an Archean anorthosite complex by continental crust

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2. Metamorphic evolution and tectonic significance of Neoarchean high-pressure mafic granulites in the Central Limpopo Belt, South Africa;International Geology Review;2023-06-28

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