Reddening of ~2.5 Ga granitoid by high-temperature fluid linked to mafic dyke swarm in the Bundelkhand Craton, north central India-Reference-Cited by-同舟云学术

Reddening of ~2.5 Ga granitoid by high-temperature fluid linked to mafic dyke swarm in the Bundelkhand Craton, north central India

Published:2017-07-04 Issue:4 Volume:53 Page:1338-1353
ISSN:0072-1050
Container-title:Geological Journal
language:en
Short-container-title:Geological Journal

Author:

Sensarma Sarajit¹^ORCID,Matin Abdul²^ORCID,Paul Debajyoti³,Patra Abhijit²,Madhesiya Abhishek Kumar¹,Sarkar Goutam²

Affiliation:

1. Centre of Advanced Study in Geology; University of Lucknow; Lucknow India

2. Department of Geology; University of Calcutta; Kolkata India

3. Department of Earth Sciences; Indian Institute of Technology; Kanpur India

Funder

Council of Scientific and Industrial Research

Publisher

Wiley

Subject

Geology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/gj.2960/fullpdf

Reference74 articles.

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3. Role of Bundelkhand granite massif and the Son-Narmada megafault in Precambrian crustal evolution and tectonism in Central and Western India;Basu;Journal of Geological Society of India,2007

4. Proterozoic crustal scale shearing in the Bundelkhand massif with special reference to quartz reefs;Bhattacharya;Journal of Geological Society of India,2013

5. Bodes , M. 1998 A report on study of I and S types of granite from part of the southern Uttar Pradesh compilation, Geological society of India, northern region, Lucknow

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