Origin of vesuvianite-garnet veins in calc-silicate rocks from part of the Chotanagpur Granite Gneiss Complex, East Indian Shield: The quantitative P-T-XCO2 topology in parts of the system CaO-MgO-Al2O3-SiO2-H2O-CO2 (+Fe2O3, F)
Author:
Affiliation:
1. Department of Geological Sciences, Jadavpur University, Kolkata 700032, India
Publisher
Mineralogical Society of America
Subject
Geochemistry and Petrology,Geophysics
Link
https://pubs.geoscienceworld.org/msa/ammin/article-pdf/104/5/744/4685129/am-2019-6811.pdf
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1. Proterozoic mobile belts-magmatism, metamorphism, geochronology and tectonics in the context of formation of the Greater Indian Landmass;Proceedings of the Indian National Science Academy;2024-04-15
2. Impact of chlorite dehydration on intermediate-depth earthquakes in subducting slabs;Communications Earth & Environment;2023-12-26
3. Competing Roles of Evolving P–T Conditions, Equilibration Volume and Chemical Potential Landscape in the Formation of Corona Texture: a Case Study from the Southern Granulite Terrane, India;Journal of Petrology;2023-11-21
4. On the factors controlling the incorporation of aluminium within titanites: a case study from medium pressure calc-silicate granulites in parts of the East Indian shield;Mineralogy and Petrology;2023-04-25
5. Formation of aluminous clinopyroxene-ilmenite-spinel symplectic assemblage in a regionally metamorphosed calc-silicate granulite from the Chotanagpur Granite Gneiss Complex, East Indian shield;Lithos;2023-04
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