Neoarchean tectonothermal imprints in the Rengali Province, eastern India and their implication on the growth of Singhbhum Craton: evidence from zircon U-Pb SHRIMP data

Author:

Bose S.1,Das K.2,Kimura K.2,Hidaka H.2,Dasgupta A.1,Ghosh G.1,Mukhopadhyay J.1

Affiliation:

1. Department of Geology; Centre for Advanced Study; Presidency University; Kolkata West Bengal 700 073 India

2. Department of Earth and Planetary Systems Science; Hiroshima University; Higashi-Hiroshima 739 8526 Japan

Funder

Council for Scientific and Industrial Research

Publisher

Wiley

Subject

Geochemistry and Petrology,Geology

Reference80 articles.

1. New U-Pb zircon ages from Paleo-Mesoarchean TTG gneisses of the Singhbhum craton, Eastern India;Acharyya;Geochemical Journal,2010

2. Late Proterozoic charnockite in Orissa, India: a U-Pb and Rb-Sr isotopic study;Aftalion;The Journal of Geology,1988

3. The effects of temperature and fO2 on the Al-in hornblende barometer;Anderson;American Mineralogist,1995

4. 2.8 Ga old anorogenic granite-acid volcanics association from western margin of the Singhbhum-Orissa craton, Eastern India;Bandyopadhyay;Gondwana Research,2001

5. On the northern margin of the Eastern Ghats in Orissa;Banerji;Records of the Geological Survey of India,1987

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