Extremely high-temperature calcareous granulites from the Eastern Ghats, India; evidence for isobaric cooling, fluid buffering, and terminal channelized fluid flow

Santanu Kumar Bhowmik; Somnath Dasgupta; Stephan Hoernes; Prasanta Kumar Bhattacharya

Santanu Kumar Bhowmik;

Santanu Kumar Bhowmik

Jadavour University, Department of Geological Sciences, Calcutta, India

Search for other works by this author on:

GSW

Google Scholar

Somnath Dasgupta;

Somnath Dasgupta

Search for other works by this author on:

GSW

Google Scholar

Stephan Hoernes;

Stephan Hoernes

Search for other works by this author on:

GSW

Google Scholar

Prasanta Kumar Bhattacharya

Search for other works by this author on:

GSW

Google Scholar

Santanu Kumar Bhowmik

Jadavour University, Department of Geological Sciences, Calcutta, India

Somnath Dasgupta

Stephan Hoernes

Prasanta Kumar Bhattacharya

Publisher: Deutsche Mineralogische Gesellschaft, Sociedad Española de Mineralogia, Societá Italiana di Mineralogia e Petrologia, Société Francaise de Minéralogie

First Online: 02 Mar 2017

Online Issn: 1617-4011

Print Issn: 0935-1221

European Journal of Mineralogy (1995) 7 (3): 689–703.

You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

Extremely high-temperature calcareous granulites from the Eastern Ghats, India; evidence for isobaric cooling, fluid buffering, and terminal channelized fluid flow

First Page Preview

Email alerts

Citing articles via

About GSW

Resources

Explore

Connect

Extremely high-temperature calcareous granulites from the Eastern Ghats, India; evidence for isobaric cooling, fluid buffering, and terminal channelized fluid flow

First Page Preview

Email alerts

Citing articles via

About GSW

Resources

Explore

Connect

This Feature Is Available To Subscribers Only