The origin of chloritoid - 3-mica pseudomorph growth in staurolite-muscovite schist, Bangriposi (Eastern India)-Reference-Cited by-同舟云学术

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The origin of chloritoid - 3-mica pseudomorph growth in staurolite-muscovite schist, Bangriposi (Eastern India)

Published:2016-05-10 Issue:5 Volume:34 Page:463-482
ISSN:0263-4929
Container-title:Journal of Metamorphic Geology
language:en
Short-container-title:J. Metamorph. Geol.

Author:

Prabhakar N.¹,Bhattacharya A.²,Mukherjee P. K.³

Affiliation:

1. Department of Earth Sciences; Indian Institute of Technology Bombay; Mumbai Maharashtra 400076 India

2. Department of Geology and Geophysics; Indian Institute of Technology; Kharagpur West Bengal 721302 India

3. Wadia Institute of Himalayan Geology; Dehradun Uttarakhand 248001 India

Funder

CPDA

Indian Institute of Technology, Kharagpur

DST

Publisher

Wiley

Subject

Geochemistry and Petrology,Geology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/jmg.12189/fullpdf

Reference99 articles.

1. Mass transfer during Barrovian metamorphism of pelites, south-central Connecticut. I. Evidence for changes in composition and volume;Ague;American Journal of Science,1994a

2. Mass transfer during Barrovian metamorphism of pelites, south-central Connecticut. II: channelized fluid flow and the growth of staurolite and kyanite;Ague;American Journal of Science,1994b

3. Deep crustal growth of quartz, kyanite and garnet into large aperture, fluid-filled fractures, north-eastern Connecticut, USA;Ague;Journal of Metamorphic Geology,1995

4. Simple models of coupled fluid infiltration and redox reactions in the crust;Ague;Contributions to Mineralogy and Petrology,1998

5. Extreme channelization of fluid and the problem of element mobility during Barrovian metamorphism;Ague;American Mineralogist,2011

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