马南区塔勒-塔勒库路段沿贝沙哈尔-查梅路的地质研究

P. Luitel, S. Panthee
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引用次数: 0

摘要

马南区塔尔至塔列库段缺乏详细的地质研究。本研究进行了1:5万比例尺的地质填图,并编制了地质剖面和岩石地层柱。研究区域部分位于高喜马拉雅结晶层和西藏特提斯层序。塔尔—塔勒库高喜马拉雅群主要由强至弱钙质片麻岩、混染片麻岩、石英岩、花岗岩等组成。它们被命名为钙硅酸盐片麻岩和副片麻岩以及正长麻岩和花岗岩单元。西藏特提斯的最下层由含有硅酸盐和长石的变质钙质岩石组成,因此该单元被称为大理石和钙片麻岩。该剖面厚度约为9公里,在许多地方存在火成岩,高度变形。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Geological study in Tal - Talekhu section of Manang District along the Besisahar – Chame Road
The section between Tal to Talekhu of Manang District lacks the detailed geological study. The geological mapping in the scale of 1:50,000 followed by the preparation of geological cross-section and lithostratigraphic column has been done in the present study. The studied area lies partially in the Higher Himalayan Crystalline and the Tibetan Tethys Sequence. The units of the Higher Himalayan Group from Tal to Talekhu consists mainly of vigorous to faintly calcareous gneiss, migmatitic gneiss, quartzite, granite, etc. They are named as the Calc. Silicate Gneiss and Paragneiss and the Orthogneiss and Granite units. The lowermost part of the Tibetan Tethys consisted of metamorphosed calcareous rocks containing silicates and feldspar, so this unit is termed as the Marble and Calc. Gneiss. The section is about 9 km in thickness and is highly deformed with presence of igneous rocks at many places.
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