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• W2034285589 abstract "Abstract The gravity field in the Nepalese Himalayas-Tsangpo region has been analysed along a profile starting from near Giridih (24°10'N, 86°20°E) and continuing over the Indian peninsular shield to near Tingri (28°50'N, 87°E) close to the Tsangpo Suture. The profile passes through the Ganga basin, Lower, Higher and Tethys Himalayas and finishes near the Indus-Tsangpo Suture. Explosion Seismology data obtained by Hirn et al. in the Himalaya-Tibetan region of Nepal has been used to restrict Moho depth along the profile. The model presented suggests that the density contrast between the crustal root beneath the High Himalaya-Tibet region and the Moho is of the order of 0.32 g cm 3 . The upper mantle should have a density of about 3.32 g cm 3 . The upper crust in the High Himalayas region appears to have higher than normal density, as compared to the crust south of the Indus-Tsangpo Suture. The model does not support continental underthrusting of the Indian plate underneath Tibet in the manner envisaged by Powell and Conaghan. The concept of lithospheric flexure underneath mountain ranges as proposed by Karner and Watts, although generally valid, does not explain the behaviour of the Moho underlying the High Himalayas in Nepal and the Tibetan Plateau, when examined in detail." @default.
• W2034285589 created "2016-06-24" @default.
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• W2034285589 date "1988-03-01" @default.
• W2034285589 modified "2023-09-23" @default.
• W2034285589 title "Analysis of the gravity field in the Nepalese Himalayas-Tibetan region in the light of plate tectonics" @default.
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• W2034285589 doi "https://doi.org/10.1016/0040-1951(88)90147-3" @default.
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