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Crustal Evolution of Bundelkhand Craton in Archean and Comparison with Other Indian Cratons

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Geological and Geo-Environmental Processes on Earth

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Abstract

Indian Shield consists of Bundelkhand, Aravalli, Singhbhum, Bastar, Western and Eastern Dharwar Cratons. The crustal evolutions of these cratons (except Singhbhum Craton) show that geodynamic mechanisms, similar to modern plate-tectonic and mantle-plume mechanisms, were active during Paleo-Neoarchean time. The Mesoarchean crustal evolution of the Bundelkhand Craton show subduction–accretion processes, which is different from other cratons of Indian Shield, whereas in other cratons, plume processes were more active during this period. During the Neoarchean period (2.7–2.5 Ga), all the cratons exhibit subduction–accretion processes. Each of the cratons demonstrates its own crust formation model. It gives the impression that the cratons of Indian Shield were parts of the Kenorland Supercontinent in Mesoarchean time, rather than one block.

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Acknowledgements

The work was supported by DST-RFBR (INT/RUS/RFBR/P-279 and RFBR-17-55-45005 IND) grants, it continues under MOU between Bundelkhand University, Jhansi, India and the Institute of Geology, Karelian Research Centre, RAS, Petrozavodsk, Russia, and is a contribution to Project AAAA-A18-118020290085-4. We thank Dr. Sanjeet Verma and Vivek Malviya for their valuable comments and criticism which seriously helped in improving this paper.

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Slabunov, A.I., Singh, V.K. (2021). Crustal Evolution of Bundelkhand Craton in Archean and Comparison with Other Indian Cratons. In: Shandilya, A.K., Singh, V.K., Bhatt, S.C., Dubey, C.S. (eds) Geological and Geo-Environmental Processes on Earth. Springer Natural Hazards. Springer, Singapore. https://doi.org/10.1007/978-981-16-4122-0_4

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