Calculation of the CO2 Degassing during Contact Metamorphism and Its Geological Significance: The Model and Example from the Shuanshan Area of the South Tan-Lu Fault Belt-Reference-Cited by-同舟云学术

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Calculation of the CO2 Degassing during Contact Metamorphism and Its Geological Significance: The Model and Example from the Shuanshan Area of the South Tan-Lu Fault Belt

Published:2010-09-07 Issue:3 Volume:82 Page:562-576
ISSN:1000-9515
Container-title:Acta Geologica Sinica - English Edition
language:en
Short-container-title:

Author:

Xiaoyong YANG,Deliang LIU,Yongjian CHEN,Jinxing DAI

Publisher

Wiley

Subject

Geology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1755-6724.2008.tb00607.x/fullpdf

Reference62 articles.

1. A model for coupled fluid flow and mixed volatile mineral reactions with applications to regional metamorphism;Baumgartner;Contribution to Mineralogy and Petrology,1991

2. Internally-consistent thermodynamic data for minerals in the system Na2O-K2 O- CaO- MgO- FeO- Fe2O3- Al2O3- SiO2- TiO2- H2O- CO2;Berman;Journal of Petrology,1988

3. Veins and hydrothermal fluid flow in the Mt. Whaleback Iron Ore District, eastern Hamersley Province, Western Australia;Brown;Precambrian Research,2004

4. A preliminary study on the relationship between the Tancheng-Lujiang fault system and mantle-derived magmatogenetic CO2 in east China;Yongjian;Geology-Geochemistry,1999

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