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The Tibetan Plateau and the Himalayan region formed after 55–50 Ma, as a result of the intracontinental collision of the Indian and Eurasian plates, occupying the east–west trending, high‐altitude Himalaya and Karakorum ranges in the south and the vast Tibetan Plateau to the north of central Asia. The tectonic evolution of Tibet began between the late Palaeozoic and the Cenozoic, and the Himalayan...
A molasse sequence comprising 1.5‐km‐thick sediments of the Lower and Middle Siwaliks Group in the sub‐Himalayan North Belt along the Tinau Khola River in west‐central Nepal was studied for the low‐field magnetic susceptibility and anisotropy using single core specimens of siltstone/sandstone from 127 stratigraphic levels. The magnetic fabric comprises primary sedimentary‐compactional and secondary...
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