Abstract:In Meghalaya, coal is present in the Lakadong sandstone formation (25 to 250 meters thick) of the Eocene epoch. The three major clusters of coalfields in Meghalaya are the Garo Hills, Khasi Hills, and Jaintia Hills. Based on petrographic studies, tectonics, and sulphur content, done by many scientists, it has been suggested that the coal-bearing strata of Jaintia Hills were formed from swamp forest on the platform areas and repeatedly subjected to marine transgression and regression. The present investigation … Show more
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