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• W2889898186 abstract "Geometry and kinematics of a hitherto ignored crustal scale tectonic discontinuity from the west-central sector of the Himalaya, viz. the North Almora Fault (NAF) is discussed in this paper. Choice of the tectonic model for response of the Himalayan-South Tibetan ensemble to the Tertiary Himalayan continental collision is largely dictated inter alia by the geometry and kinematics of the large orogen parallel strike slip faults in the region. Based on field, laboratory and satellite imagery data, it is concluded that the North Almora Fault/Thrust is not one but two closely parallel tectonic discontinuities viz. (i) the North Almora Fault, a steep south dipping high angle brittle fault with a dominant east slip and subordinate dip slip component and (ii) the North Almora Thrust, a low angle south dipping thrust marking the northern boundary of the large Almora - Jajarkot Nappe. The >500 km long dextral strike slip North Almora Fault mimicking the ∼800 km long Karakoram Fault is responsible for significant strain partitioning in the west-central Lesser Himalaya. The North Almora Fault assumes special salience for the Himalayan tectonics as it partitions sizable strains in addition to the Karakoram Fault in the region and lends support to the oblique convergence model that best describes the Himalayan extensional and strike slip deformation." @default.
• W2889898186 created "2018-09-27" @default.
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• W2889898186 date "2019-04-01" @default.
• W2889898186 modified "2023-10-16" @default.
• W2889898186 title "North Almora Fault: A crucial missing link in the strike slip tectonics of western Himalaya" @default.
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• W2889898186 doi "https://doi.org/10.1016/j.jseaes.2018.09.002" @default.
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