Abstract
North fringe of Ganga foreland basin; subsurface structure of Terai; Dang and Deukhuri intermontane valleys; fluvial terraces of Dang; sediments of Pokhara and neighborhood; Begnas Formation, Siswa Formation, Tallakot Formation; Ghachok Formation, Pokhara Formation, and Phewa Formation; origin of lakes in Pokhara Valley and tectonic implications; Kathmandu basin fill; Lukundol Formation, Pyanggaon Terrace Deposit, Chapagaon Terrace Deposit, Boregaon Terrace Deposit, Dharmasthai Formation, Gokarna Formation, Tokha Formation, Thimi Formation, Kalimati Formation, Patan Formation, and Lower Terrace Deposit; paleoclimate in Kathmandu Valley; Thakkhola–Mustang graben; Thakmar series; Tetang Formation, Thakkhola Formation; Sammargaon Formation; Marpha Formation; Dangarjong normal fault; tectonic and environmental interpretations.
The lack of isostatic equilibrium and the existence of very smooth, inclined substratum suggest that the Himalayas are currently under the influence of large scale tectonic forces, probably due to collision of the Indian plate against the Asian plate.
—Kono (1974, p. 283)
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Dhital, M.R. (2015). Terai and Intermontane Basins. In: Geology of the Nepal Himalaya. Regional Geology Reviews. Springer, Cham. https://doi.org/10.1007/978-3-319-02496-7_34
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