A contribution to the geology of the Annapurna and Nilgiri Himals, Nepal
A contribution to the geology of the Annapurna and Nilgiri Himals, Nepal
复制标题
对尼泊尔安纳布尔纳山和尼尔吉里山地质学的贡献
作者：
A. Waltham
在尼泊尔中西部的特提斯地区，尼尔吉里石灰岩是主要的单位。根据新发现的露头，对拉戎组分离的意义提出了质疑，并对尼尔吉里砂岩进行了描述。安娜普尔纳、尼尔吉里和道拉吉里之间有卧褶构造对比。在这些山脉之间，Thakkhola地堑断层继续向南延伸，并对其抛出的幅度进行了估计。
Summary Within the Tethyan Zone of Central West Nepal, the Nilgiri Limestone is the dominant unit. The significance of the separation of the Larjung Formation is questioned in the light of new outcrops examined, and the Nilgiri Sandstone is described. Recumbent fold structures are correlated between Annapurna, Nilgiri and Dhaulagiri. Between these mountains the Thakkhola graben faults are continued southwards, and estimates are made of the magnitude of their throws.