Petrotectonic framework of granitoids and associated granulites at Nagavalli Shear Zone (NSZ), Eastern Ghats Belt: Evidence of a late transpression orogeny-Reference-Cited by-同舟云学术

Petrotectonic framework of granitoids and associated granulites at Nagavalli Shear Zone (NSZ), Eastern Ghats Belt: Evidence of a late transpression orogeny

Published:2015-06 Issue:4 Volume:124 Page:707-727
ISSN:0253-4126
Container-title:Journal of Earth System Science
language:en
Short-container-title:J Earth Syst Sci

Author:

Saha Tamoghna,Karmakar Subrata

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://link.springer.com/content/pdf/10.1007/s12040-015-0579-4.pdf

Reference58 articles.

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3. Bhadra S, Gupta S and Banerjee M 2004 Structural evolution across the Eastern Ghats Mobile Belt–Bastar Craton boundary, India: Hot over cold thrusting in an ancient collision zone; J. Struct. Geol. 26 233–245.

4. Bhattacharyya S, Swain A K and Teixeira W 2004 Crustal source for a syenite complex in the high-grade Eastern Ghats belt, India: Sm–Nd isotopic evidence; Gondwana Res. 7 627–629.

5. Bhowmik S K, Dasgupta S, Hoerness S and Bhattacharya P K 1995 Extremely high temperature calcareous granulites from the Eastern Ghats, India: Evidence for isobaric cooling, fluid buffering and terminal channelized fluid flow; Eur. J. Mineral. 7 689–703.

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