Peraluminous A-type granites formed through synchronous fractionation, magma mixing, mingling, and undercooling: evidence from microgranular enclaves and host Mesoproterozoic Kanigiri granite pluton, Nellore Schist Belt, southeast India-Reference-Cited by-同舟云学术

Peraluminous A-type granites formed through synchronous fractionation, magma mixing, mingling, and undercooling: evidence from microgranular enclaves and host Mesoproterozoic Kanigiri granite pluton, Nellore Schist Belt, southeast India

Published:2023-06-05 Issue:4 Volume:42 Page:603-636
ISSN:2096-0956
Container-title:Acta Geochimica
language:en
Short-container-title:Acta Geochim

Author:

Narshimha Ch.,Kumar Santosh^ORCID

Funder

University Grants Commission

Ministry of Earth Science, Govt. of India

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology

Link

https://link.springer.com/content/pdf/10.1007/s11631-023-00608-8.pdf

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4. Anderson JL, Smith DR (1995) The effects of temperature and fO2 on the Al-in-hornblende barometer. Amer Miner 80:549–559

5. Anderson JL, Barth AP, Wooden JL, Mazdab F (2008) Thermometers and thermobarometers in granitic systems. Rev Mineral Geochem 69:121–142. https://doi.org/10.2138/rmg.2008.69.4

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