Petrography, geochemistry and detrital zircon geochronology of the Srisailam Quartzite Formation, Cuddapah Basin, India: Implications for depositional age, correlation and provenance
[Display omitted] •Duration of sedimentation in the Srisailam sub-basin was > 1840 Ma ≤ 1770 Ma.•The Srisailam Formation formed in a passive margin setting.•The dominant source area for the Srisailam Formation was the Dharwar Craton.•The Srisailam Formation contains Palaeo-Mesoarchaean and traces...
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Published in | Precambrian research Vol. 387; p. 106978 |
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Main Authors | , , , , , , |
Format | Journal Article |
Language | English |
Published |
Elsevier B.V
01.04.2023
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Subjects | |
Online Access | Get full text |
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