Journal of Geological Society of India (Online archive from Vol 1 to Vol 78)

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Siliciclastic rocks around Surgutaria viIIage are mature to sub-mature quartzarenites to quartz-wackes, Quartz-wackes are produced due to extensive readjustment of sericite-chert matrix during phyllomorphic stage of development in the arenite frame work. Various statistical parameters, and current structures clearly reveal that the deposition of siliciclastics took place in a stable shallow marine to tidal flat environment.
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