Abstract:The Indian plate underthrusting the Himalaya is considered to be
segmented along the collision belt arc and seismic images of the Indian
mantle lithosphere (IML) suggest along-arc variations in the angle of
underthrusting and its northern limit beneath Tibet. The pre-existing
transverse tectonic structures of the Indian plate mapped in the Ganga
foreland basin have been related to these segmentation boundaries. These
segmentations imply changes in mechanical properties of adjoining blocks
which should manifest… Show more
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