Zircon U-Pb-Hf constraints on the geological evolution of the Bihar Mica Belt, Central Indian Tectonic Zone, and its link to Columbia assembly

Author:

Abhinay KumarORCID,Upadhyay Dewashish

Funder

Indian Institute of Technology Kharagpur

Department of Geology and Geophysics, Yale University

University Grants Commission

Publisher

Elsevier BV

Reference71 articles.

1. A plate tectonic model for Proterozoic crustal evolution of Central Indian Tectonic Zone;Acharyya;Gondwana Geol. Mag,2003

2. Paleoproterozoic mafic dyke swarms from the Dharwar craton; paleomagnetic poles for India from 2.37 to 1.88 Ga and rethinking the Columbia supercontinent;Belica;Precambr. Res.,2014

3. The growth of the continental crust: constraints from zircon Hf-isotope data;Belousova;Lithos,2010

4. Sequence of deformation, metamorphism and igneous intrusions in Bihar mica belt;Bhattacharya;Mem. Geol. Soc. India,1988

5. Petrogenesis and geochronology of the Arkasani Granophyre and felsic Dalma volcanic rocks: implications for the evolution of the Proterozoic North Singhbhum Mobile Belt, east India;Bhattacharya;Geol. Mag.,2015

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