In: Gupta HK, Delany FM (eds) Zagros-Hindu Kush-Himalaya geodynamic evolution. Ten years of research in Central Nepal Himalaya and some other regions. Tectonophysics 95:43–60īordet P, Colchen M, Le Fort P, Pêcher A (1981) The geodynamic evolution of the Himalaya. V., and United Nations Environment ProgrammeĪrita K (1983) Origin of the inverted metamorphism of the lower Himalayas, Central Nepal. Department of Mines and Geology, International Centre for Integrated Mountain Development, Carl Duisberg Gesellschaft e. thesis, submitted to the Central Department of Geology, Tribhuvan University, Kathmandu, 70 ppĪmatya KM, Jnawali BM (1994) Geological map of Nepal, Scale: 1:1 000 000. KeywordsĪdhikari DP (1993) Paleomagnetism of the dyke rocks of the Ampipal Massif, Lesser Himalaya, Central Nepal. Gandaki region with widest Lesser Himalayan belt comprising inner, intermediate, and outer zones inner zone within Great Midland Antiform, consisting of Kuncha Formation and rare nepheline syenite intrusives near Ampipal garnetiferous schists and gneisses, and graphitic schists and marbles Main Central Thrust brining Higher Himalayan crystallines over Lesser Himalayan sequence stretching and mineral lineations in Kuncha Formation dome- and basin-like folds alkali syenites of Sikkim and Chhotanagpur intermediate zone of Kusma–Syangja within core of Great Mahabharat Synform, constituted of Lower Nawakot Group, Upper Nawakot Group, Sirkot Group, and Tansen Group north- as well as south-dipping imbricate faults, constituting triangle zone Outer belt of Kali Gandaki and Palpa made up of Middle Kali Gandaki Group, Upper Kali Gandaki Group, and Tansen Group fold-and-thrust belt of Gandaki region comprising tight and recumbent folds, thrusts, backthrusts, klippen, and outliers.
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