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Soft-sediment deformation structures occur in the ~150m thick Pliocene-Quaternary fluvio-lacustrine sediments exposed around the Khalsar and Tirit areas in the lower Shyok river valley, northern Ladakh and eastern Karakoram, India. These structures vary in morphology and pattern and occur at different stratigraphic horizons. They satisfy the criteria for attributing them to seismic events and it is...
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