Geochronology, whole-rock geochemistry and Sr-Nd isotopes of the Bhanupratappur mafic dyke swarm: Evidence for a common Paleoproterozoic LIP event at 2.37–2.36 Ga in the Bastar and Dharwar cratons

Author:

Pandey Om Prakash,Mezger Klaus,Söderlund Ulf,Upadhyay Dewashish,Srivastava Rajesh K.,Gautam Gulab C.,Ernst Richard E.

Funder

Swiss National Science Foundation

Canadian NSERC CRD

Russian Mega-Grant

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference86 articles.

1. New paleomagnetic results on ~2367 Ma Dharwar giant dyke swarm, Dharwar craton, southern India: implications for Paleoproterozoic continental reconstruction;Babu;J. Earth Syst. Sci.,2018

2. Short-lived mantle generated magmatic events and their dyke swarms: the key unlocking Earth’s paleogeographic record back to 2.6 Ga. Dyke swarms–time markers of crustal evolution;Bleeker;Sci. Bull.,2006

3. A giant circumferential dyke swarm associated with the High Arctic Large Igneous Province (HALIP);Buchan;Gondwana Res.,2018

4. Giant circumferential dyke swarms: catalogue and characteristics;Buchan,2019

5. Locating South China in Rodinia and Gondwana: a fragment of greater India lithosphere?;Cawood;Geology,2013

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