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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Bibliographic Details
Main Author: Sampa Ghosh
Format: Article
Language:English
Published: Elsevier 2023-06-01
Series:Journal of Asian Earth Sciences: X
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S2590056023000142