Dynamic recrystallization mechanisms and vorticity estimation of the Terrane Boundary Shear Zone (Lakhna shear zone): Implications on dynamics of juxtaposition of the Eastern Ghats Mobile Belt with the Bastar Craton, NW Odisha

Author:

Meher Bhupesh,Behera Bhuban Mohan,Biswal Tapas Kumar

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Reference60 articles.

1. Aftalion M, Bowes D R, Dash B and Fallick A E 2000 Late Pan-African thermal history in the Eastern Ghats terrane, India, from U–Pb and K–Ar isotopic study of the Mid-Proterozoic Khariar alkali syenite, Orissa; Geol. Surv. India 57 26–32.

2. Boutonnet E, Leloup P H, Sassier C, Gardien V and Ricard Y 2013 Ductile strain rate measurements document long-term strain localization in the continental crust; Geology 41(8) 819–822.

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(2) 233–245.

4. Biswal T K 1998 The lithotectonic setting of the Eastern Ghat Mobile Belt and adjoining craton in western Orissa, India: An example of Mesoproterozoic Fold-Thrust Belt; Gondwana Res. 1 410–412.

5. Biswal T K and Sahoo D 1998 IRS-1C digital data interpretation of lithotectonic setting in northwestern part of the Eastern Ghats Mobile Belt, Orissa; Curr. Sci. 75(8) 846–850.

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