Importance of fluid immiscibility in the H2O-NaCl-CO2 system and selective CO2 entrapment in granulites: experimental phase diagram at 5-7 kbar, 900°C and wetting textures-Reference-Cited by-同舟云学术

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Importance of fluid immiscibility in the H2O-NaCl-CO2 system and selective CO2 entrapment in granulites: experimental phase diagram at 5-7 kbar, 900°C and wetting textures

Published:1998-12-01 Issue:6 Volume:10 Page:1109-1124
ISSN:0935-1221
Container-title:European Journal of Mineralogy
language:en
Short-container-title:ejm

Author:

Gibert François,Guillaume Damien,Laporte Didier

Publisher

Schweizerbart

Subject

Geochemistry and Petrology

Cited by 54 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Fluid–Melt–Rock Interaction during the Transition from Magmatism to HT-UHT-Granulite- and Amphibolite-Facies Metamorphism in the Ediacaran Adrar–Suttuf Metamafic Complex, NW Margin of the West African Craton (Southern Morocco);Journal of Petrology;2024-05-13

2. The Potential Role of Sulfur during Granulite-facies Metamorphism, Oxidation, and Geochemical Transformation of the Granitoid Lower Crust;Petrology;2024-02

3. Zircon as a Recorder of Trace Element Changes during High-Grade Metamorphism of Neoarchean Lower Crust, Shevaroy Block, Eastern Dharwar Craton, India;Journal of Petrology;2022-04-14

4. Fluid diversity in the gold-endowed Archean orogenic systems of the Abitibi greenstone belt (Canada) I: Constraining the PTX of prolonged hydrothermal systems;Ore Geology Reviews;2021-08

5. Thallium Isotopes Reveal Brine Activity During Carbonatite Magmatism;Geochemistry, Geophysics, Geosystems;2021-03

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