Petrography and geochemistry of siliciclastic sediments in Permo-Triassic transition from the southern Pranhita-Godavari Gondwana basin, India: Implications for paleoclimate
The Kamthi Formation, in the intracratonic Pranhita-Godavari Gondwana rift basin, bore signatures of climate change from a warm humid climate in Late Permian to hot arid during the Early Triassic. Sedimentation took place mainly under fluvial conditions. The Kamthi sediments were unaffected by buria...
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| Hlavní autor: | |
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| Médium: | Artigo |
| Jazyk: | Inglês |
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Elsevier
2023-06-01
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| Edice: | Journal of Asian Earth Sciences: X |
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| On-line přístup: | http://www.sciencedirect.com/science/article/pii/S2590056023000142 |
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