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Geological setting and lithostratigraphy of Bandipur-Gondrang area of Lesser Himalaya, central Nepal

机译:尼泊尔中部小喜马拉雅山Bandipur-Gondrang地区的地质环境和岩石地层学

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Detailed geological mapping was carried out in the Bandipur-Gondrang area of Tanahun district to clarify the geological set up and stratigraphy of the area. Wherever possible, geological mapping is based on stratigraphic units proposed by Stocklin and Bhattarai (1977) in central Nepal and the present mapping is the west ward continuation from Mugling-Banspani area (Paudyal and Paudel, 2011). The study area comprises low grade metasedimentary rocks of Nawakot Complex. The rock succession of the area are divided into six formations as the Kunchha Formation, the Fagfog Quartzite, the Dandagaon Phyllite, the Nourpul Formation with four members, the Dhading Dolomite and the Benighat Slates in stratigraphic upwards. The former four formations belong to Upper Nawakot Group and the remaining one belongs to the Lower Nawakot Group of Nawakot Complex (St?cklin and Bhattarai, 1977). Based on lithology, the Nourpul Formation is divided into the Purebensi Quartzite, the Amdanda Phyllite, the Labdi Khola Member and the Bandipur Slate from bottom to top respectively. The Purebensi Quartzite is lithologically distinct in the field; the Labdi Khola Member is significant with copper and iron mineralization in the area, and the Bandipur Slate is also significant with roofing quality slate, however, the Amdanda Phyllite is mapped as an intervening member between significant lithologies. The rocks of the present study area consist of several sedimentary structures like mud cracks, ripple marks, graded bedding and cross and parallel laminations. A broad Ghumaune- Gondran Synclinorium is mapped in the area. In addition to this, several anticlines and synclines are also mapped in the study area. Jalbhanjyang Thrust has brought the older metasedimentary rocks of the Nawakot Complex over the younger rocks of the same Complex. Some corrections are recommended over the distribution of previously shown lithological units by Stocklin and Bhattarai (1977) around the Ghumaune-Bhut Khola section. DOI: http://dx.doi.org/10.3126/bdg.v15i0.7417 Bulletin of the Department of Geology, Vol. 15, 2012, pp. 49-62
机译:在Tanahun区的Bandipur-Gondrang地区进行了详细的地质测绘,以弄清该地区的地质构造和地层。可能的情况下,地质测绘是基于Stocklin和Bhattarai(1977)在尼泊尔中部提出的地层单位,目前的测绘是Mugling-Banspani地区向西的延续(Paudyal和Paudel,2011)。研究区域包括纳瓦科特综合体的低品位变质沉积岩。该地区的岩层划分为6个地层,分别是Kunchha组,Fagfog石英岩,Dandagaon Phyllite,具有4个成员的Nourpul组,Dhading白云岩和Benighat板岩。前四个编队属于上纳瓦科特集团,其余四个属于纳瓦科特综合体的下纳瓦科特集团(St?cklin和Bhattarai,1977年)。根据岩性,从下至上分别将努尔普尔岩层分为Purebensi石英岩,Amdanda辉石岩,Labdi Khola成员和Bandipur板岩。 Purebensi石英岩在该领域在岩性上是不同的。 Labdi Khola成员对于该地区的铜和铁矿化具有重要意义,Bandipur板岩对于屋顶质量板岩也具有重要意义,但是,Amdanda Phyllite被映射为重要岩性之间的中间成员。本研究区的岩石由几种沉积结构组成,如泥裂,波纹痕迹,渐变层理以及交叉和平行叠片。该地区绘制了宽阔的Ghumaune- Gondran Synclinorium。除此之外,研究区域还绘制了一些背斜线和向斜线。 Jalbhanjyang Thrust将Nawakot综合体的较旧的沉积沉积岩带入了该综合体的较年轻的岩石。 Stocklin和Bhattarai(1977)在Ghumaune-Bhut Khola剖面附近对先前显示的岩性单元的分布提出了一些校正建议。 DOI:http://dx.doi.org/10.3126/bdg.v15i0.7417地质学部公告,第一卷2012年15月,第49-62页

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