Detrital zircon U–Pb LA‐ICPMS ages from the Kolhan Group, Singhbhum Craton, eastern India: Implications for terminal Mesoproterozoic palaeogeography between Columbia and Rodinia along the Central Indian Tectonic Zone

Author:

Mukhopadhyay Joydip1ORCID,Crowley Quentin2,Ghosh Bhaskar13,Ghosh Gautam1,Heron Kyle2

Affiliation:

1. Department of Geology Presidency University Kolkata India

2. Department of Geology School of Natural Sciences, Trinity College Dublin 2 Ireland

3. Department of Geology Jogamaya Devi College Kolkata India

Funder

DST, India

FEMS project fund to QGC, JM and GG from Trinity College Dublin

FRPDF, Presidency University, kolkata

Publisher

Wiley

Subject

Geology

Reference164 articles.

1. The Daitari‐Tomka Basin – Its structural and stratigraphic evolution & genesis of associated iron ores;Acharya S.;Indian Journal of Geology,2002

2. Greenstones from Singhbhum Craton, their Archaean character, oceanic crustal affinity and tectonics;Acharyya S. K.;Proceedings National Academy of Science, India,1993

3. Evolutionary characters of the Gondwanic Indian crust;Acharyya S. K.;Indian Minerals,1997

4. The Nature of Mesoproterozoic Central Indian Tectonic Zone with Exhumed and Reworked Older Granulites

5. New U-Pb zircon ages from Paleo-Mesoarchean TTG gneisses of the Singhbhum Craton, Eastern India

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