Geological Study of the Lesser Himalaya in the Kusma-Baglung Area, Western Nepal

N. Sapkota, L. Paudel
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Abstract

Geological study was carried out along the Kaligandaki and Modi Khola valleys in west Nepal. The area comprises the rock of Lesser Himalayan metasedimentary sequence. Main rock types present in the area are quartzite, phyllite, metasandstone and psammatic phyllite. Schist and gneiss are present in some parts. Ulleri Gneiss is explored in the area. Kusma-Baglung area comprises the spectacular terrace deposits formed at the Quaternary time by the Kaligandaki River and the Modi Khola. The terrace extensively comprises clast of limestone, marble, gneiss, quartzite, schist, phyllite ranging in size from fine matrix to huge boulders derived from the Higher Himalaya. Bulletin of Department of Geology, vol. 20-21, 2018, pp: 29-36
尼泊尔西部库斯马-巴格隆地区小喜马拉雅的地质研究
地质研究沿着尼泊尔西部的Kaligandaki和Modi Khola山谷进行。该地区包括小喜马拉雅变质沉积层序的岩石。区内主要岩石类型为石英岩、千层岩、变质砂岩和泥质千层岩。部分地区有片岩和片麻岩。该地区勘探了乌列里片麻岩。库斯马-巴格隆地区由Kaligandaki河和Modi Khola河在第四纪形成的壮观的阶地矿床组成。阶地主要由石灰岩、大理岩、片麻岩、石英岩、片岩、千层岩等碎屑组成,大小从细粒基质到源自高喜马拉雅的巨砾不等。地质通报,2018年第20-21卷,pp: 29-36
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