Metamorphic P – T – t – d evolution of the Mesoproterozoic Pur‐Banera supracrustal belt, Aravalli Craton, northwestern India: Insights from phase equilibria modelling and zircon–monazite geochronology of metapelites-Reference-Cited by-同舟云学术

Metamorphic P – T – t – d evolution of the Mesoproterozoic Pur‐Banera supracrustal belt, Aravalli Craton, northwestern India: Insights from phase equilibria modelling and zircon–monazite geochronology of metapelites

Published:2021-05-04 Issue:9 Volume:39 Page:1173-1204
ISSN:0263-4929
Container-title:Journal of Metamorphic Geology
language:en
Short-container-title:J Metamorph Geol

Author:

D’Souza Joseph¹²^ORCID,Prabhakar N.¹^ORCID,Sheth Hetu¹,Xu Yigang³

Affiliation:

1. Department of Earth Sciences Indian Institute of Technology Bombay Powai India

2. Department of Applied Geology Indian Institute of Technology (Indian School of Mines) Dhanbad India

3. State Key Laboratory of Isotope Geochemistry Guangzhou Institute of Geochemistry Chinese Academy of Sciences Guangzhou China

Funder

Science and Engineering Research Board

University Grants Commission

Publisher

Wiley

Subject

Geochemistry and Petrology,Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/jmg.12606

Reference107 articles.

1. Behavior of accessory phases and redistribution of Zr, REE, Y, Th, and U during metamorphism and partial melting of metapelites in the lower crust: an example from the Kinzigite Formation of Ivrea-Verbano, NW Italy

2. Non-ideal mixing in the phlogopite-annite binary: constraints from experimental data on Mg?Fe partitioning and a reformulation of the biotite-garnet geothermometer

3. Grenvillian age high-pressure upper amphibolite-granulite metamorphism in the Aravalli-Delhi Mobile Belt, Northwestern India: New evidence from monazite chemical age and its implication

4. Orogeny, migmatites and leucogranites: A review

5. Constraints on the Proterozoic evolution of the Aravalli–Delhi Orogenic belt (NW India) from monazite geochronology and mineral trace element geochemistry

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