![]() Bull Dep Geol Tribhuvan Univ Kathmandu 2(1):11–23 Koide Y, Arita K, Toyoshima T, Sharma MP (1992) Geochemistry of Ampipal pluton, preliminary report. Bull Natl Sci Mus Tokyo Ser C 11(4):141–153 Kimura T, Bose MN, Sakai H (1985) Fossil plant remains from Taltung Formation, Palpa district, Nepal Lesser Himalaya. ![]() Hirayama J, Nakajima T, Shrestha SB, Adhikari TP, Tuladhar RM, Tamrakar JM, Chitrakar GR (1988) Geology of southern part of the Lesser Himalaya, west Nepal. Denkschiiften der Schweizerischen Naturforschenden Gesellschaft, Band LXXXVI/1, 185 pp (with a geological map) Hagen T (1969) Report on the geological survey of Nepal. Goswami B, Bhattacharya C (2008) Metamorphism of nepheline syenite gneisses from Chhotanagpur Granite Gneiss complex, Northeastern Puruliya district, Eastern India. thesis submitted to the Hokkaido University, Sapporo, Japan, 165+ pp Gautam P (1990) Paleomagnetic study of the Lesser Himalaya in Nepal. Gautam P, Koshimizu S (1991) Zircon and apatite fission-track dating of the Ampipal Alkaline Massif, the Nepal Lesser Himalaya. ![]() Jahrbuch der Geologischen Bundesanstalt 18:1–103 (with a geological map and cross-sections) United Nations, New York, 107 pp (with a geological map in colors)įuchs G, Frank W (1970) The geology of west Nepal between the rivers Kali Gandaki and Thulo Bheri. Bull Dep Geol Tribhuvan Univ 9(Special Issue):1–60ĮSCAP (Economic and Social Commission for Asia and the Pacific) (1993) Geology and mineral resources of Nepal, atlas of mineral resources of the ESCAP region, vol 9. J Nepal Geol Soc 11(Special Issue):159–170ĭhital MR, Thapa PB, Ando H (2002) Geology of the inner Lesser Himalaya between Kusma and Syangja in western Nepal. American Geophysical Union, Washington, DC, pp 149–168ĭhital MR (1995) Mode of occurrence of nepheline syenites in the Gorkha–Ampipal area, Central Nepal Lesser Himalaya. 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. ![]() Try before you buy? Order a sample of this aggregate belowįREE DELIVERY!* Free delivery to most U.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. Whilst this can look different to product, it also adds character and offers a very natural look and feel. It has a flat angular shape, buff when dry yet glossy when wet.ĭisclaimer – A natural process of oxidation can occur on this decorative stone, it may appear to look slightly rusty, this is completely natural and can be caused by several external factors such as, weather, pets, ground laid on or general change in environment. This multi-purpose aggregate can be used for mulching borders, driveways, and landscaping, also Ideal for filling in between patio slabs. Our green slate evokes calm and serenity, this clean green slate sits happily in both contemporary settings and classic gardens alike. ![]()
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