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- W4383374988 abstract "The sedimentary sequence of the Barail Group preserves the records of the depositional history of Indo-Myanmar Range during Eocene–Oligocene. Field investigation, geochemistry and detrital geochronology are used to study its geochemical characteristics, sediment provenance, paleoweathering condition, and tectonic setting. Major elements-based discrimination plots indicate that the sediments of this group were derived from quartzose sedimentary sources and were deposited in an active continental margin tectonic set-up. Barail sandstone displays a gentle sloping LREE and more or less flat HREE pattern and shows negative Eu anomaly and positive Sm anomaly. Paleoweathring indices indicate Barail sediments have undergone moderate to high weathering before deposition. Detrital zircon U–Pb reveal ages ranging from 3225 to 90 Ma, with clusters at 222–90 Ma, 1215–394 Ma, 1849–1364 Ma, 2500–2094 Ma and 3225–2094 Ma. These results indicate the majority of the sediments of the Barail Group of Indo-Myanmar Range were sourced from the Tethyan Sedimentary Sequence and Trans-Himalayan granitoids. They were deposited in shallow marine to deltaic environment and were deposited by the Brahmaputra River system." @default.
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- W4383374988 date "2023-07-06" @default.
- W4383374988 modified "2023-09-26" @default.
- W4383374988 title "Geochemistry and detrital geochronology of sandstones of Barail Group of Indo-Myanmar Range, NE India" @default.
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- W4383374988 doi "https://doi.org/10.1007/s43217-023-00142-w" @default.
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