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- W2530999953 abstract "Source-signature imbibed within geochemistry and detrital mineralogy gets blurred when correlated with physical characteristics in the Barremian-Aptian siliciclastic-fill of the Pondicherry Sub-basin, India. Six alluvial conglomerate-shale facies associations linked with paleocurrent patterns present a facsimile of basin-margin scree/alluvial fans transiting into a low-sinuosity axial river system, in turn passing into a distal floodplain traversed by high-sinuosity channel branches. The QFL-plot for the sandstones indicates cratonic source gaining relative maturity toward the distal depositional setting. Geochemical data clearly document variable degrees of mixing of felsic and mafic components, and source-shifting in concert with rifting. Weathering had been moderate with an annual temperature around 12°C and rainfall 844–1060 mm, although geophysical reconstructions suggest high paleolatitude. Intrabasinal sediment transport and diagenesis, nonetheless, left a noteworthy overprint." @default.
- W2530999953 created "2016-10-21" @default.
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- W2530999953 date "2017-01-01" @default.
- W2530999953 modified "2023-09-25" @default.
- W2530999953 title "Physico-Chemical Characteristics of the Barremian-Aptian Siliciclastic Rocks in the Pondicherry Embryonic Rift Sub-basin, India" @default.
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- W2530999953 doi "https://doi.org/10.1016/b978-0-12-803386-9.00006-x" @default.
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