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

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Signatures of active tectonics have been observed in the eastern part of Doon valley in proximity to a lineament (fault?) cutting across the Himalayan grain. A normal fault has been observed over the Doon sediments represented by a sequence of silty clay, gravel and clay exposed in a quarry section. The fault displaces the litho sequence with a vertical throw of 1 5 m. This suggests tectonic movement along the fault during Quaternary period.

Keywords

Neotectonics, Quaternary, Doon Valley, Uttaranchal.
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