作者: A. K. Jain , D. M. Banerjee , Vivek S. Kale
DOI: 10.1007/978-3-030-42845-7_5
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摘要: The Banded Gneiss Complex attached to the Aravalli Craton in west with coeval Bundelkhand center, Singhbhum and Meghalaya Cratons east, Bastar Dharwar cratons south constitute Precambrian nuclei of Peninsular India.