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- W2247253044 abstract "Diagenetic changes and depositional history of the Damuda sandstone of a part of DarjeeJing Himalaya is described. The sandstones are classified as quartzitic and non-quartzitic on the basis of their physical characters. The quartzitic sandstones occur along the entire length of Precambrian Daling metamorphics as a thin zone whereas the non-quartzitic sandstones occupy the major part of the field. The characters exhibited by the non-quartzitic sandstones indicate diagenetic conditions but in case of quartzitic sandstones it cannot be said with certainty. Possibly dynamic metamorphism caused by Daling thrust has had a role in bringing about the changes." @default.
- W2247253044 created "2016-06-24" @default.
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- W2247253044 date "1976-03-01" @default.
- W2247253044 modified "2023-09-23" @default.
- W2247253044 title "Depositional History of Damuda Sandstone in Lish-Ramthi Valley, Darjeeling District" @default.
- W2247253044 hasPublicationYear "1976" @default.
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