The evolution of Archean crust undisturbed for three billion years: A case study from the Bahalda Pluton, Singhbhum Craton, eastern India

Author:

Gumsley Anna,Słaby Ewa,Dey Sukanta,Chew David,Gmochowska Wiktoria,Wudarska Alicja,Gumsley Ashley,Szopa Krzysztof,Krzykawski Tomasz,Marciniak-Maliszewska Beata,Drakou Foteini

Funder

Narodowe Centrum Nauki

Instytut Nauk Geologicznych Polskiej Akademii Nauk

Science Foundation Ireland

Publisher

Elsevier BV

Reference73 articles.

1. A plume-mantle interaction model for the petrogenesis of komatiite-komatiitic basalt-basalt-basaltic andesite volcanism from the Paleoarchean (3.57-3.31 Ga) Iron Ore Group greenstone belts, Singhbhum craton, India: Constraints from trace element geochemi;Adhikari;Lithos,2021

2. Petrogenesis of the Mesoarchean (∼3.05 Ga) mafic volcanics from the western Iron Ore Group volcano-sedimentary succession, Singhbhum craton, eastern India: constraints from geochemical modelling and Sm-Nd geochronology;Adhikari;Lithos,2022

3. U-Pb geochronology of zircon and polygenetic titanite from the Glastonbury Complex, Connecticut, USA: an integrated SEM, EMPA, TIMS, and SHRIMP study;Aleinikoff;Chem. Geol.,2002

4. Ages and origins of rocks of the Killingworth dome, south-central Connecticut: Implications for the tectonic evolution of southern New England;Aleinikoff;Am. J. Sci.,2007

5. Summary of recommendations of AIPEA nomenclature committee on clay minerals;Bailey;Am. Miner.,1980

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