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尼泊尔喜马拉雅地区的新构造运动和地球动力学的主要特征可以由本区的构造地势和构造基础面很好地表示出来。本地区山脉结构在横向上的划分与地质学上依构造特征而划分出来的单元相一致;在纵向上,则按照构造运动形成的不同山口将山脉划分为几段。由多个推覆体板片和形成众多Si walik期山前褶皱的印度次大陆俯冲断层构成的体系展示了喜马拉雅新构造动力学的主要过程。伴随这一动力学过程,出现了Mahabharat地区向斜核部地层被挤出及推覆体露头被剥蚀、喜马拉雅地区高倾斜基础面重力不稳性、整个喜马拉雅地区花岗岩岩基呈漂浮状态等地质现象。
Neotectonic movement and geodynamics in the Himalayas, Nepal, can be characterized by tectonic topography and tectonic basement in this area. The lateral division of the mountain range structure in the region is consistent with the unit geologically categorized according to the tectonic features. In the vertical direction, the mountain ranges are divided into sections according to the different mountain passes formed by tectonic movements. A system of multiple nappe plates and subducted Indian subcontinent faults that form many Siwalik foreland folds demonstrates the major process of neotectonic dynamics in the Himalayas. Accompanying this kinetic process are the geological phenomena of the outcropping of the syncline core in the Mahabharat region and the denudation of outcrops, the gravitational instability of the highly tilted basement surface in the Himalayas and the floating uplift of the granite basement throughout the Himalayas .