A review of the ∼1600 Ma sedimentation, volcanism, and tectono-thermal events in the Singhbhum craton, Eastern India
The Palaeoproterozoic–Mesoproterozoic transition (∼1600 Ma) is a significant event in the Earth history as a global thermal perturbation affected the pre-1600 Ma landmasses. Like other cratonic blocks of the world, lithospheric thinning, sedimentation, magmatism, metamorphism and crustal melting/ana...
Main Authors: | , , , , |
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Format: | Article |
Language: | English |
Published: |
Elsevier
2013-05-01
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Series: | Geoscience Frontiers |
Subjects: | |
Online Access: | http://www.sciencedirect.com/science/article/pii/S1674987112001326 |