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In the Trans-Himalaya, the Trans-Himadri fault (THF) controlled the extent of past glaciers. The rivers were impounded by glacial debris resulting in the formation of lakes that recorded regional climatic and seismic events. One such lake formed at Garbayang, where the upper 28 m lacustrine succession spanned an age range of 20–10 ka. Magnetic susceptibility and sedimentological data suggest that...
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