新疆喀喇昆仑岔路口构造浅析

The fork structure in Xinjiang

新疆喀喇昆仑山属燕山褶皱系,大地构造的发育主要与南亚次大陆向北位移并与欧亚大陆碰撞有关。主要大地构造期始于白垩纪,继续到第三纪;山地抬升开始于晚第三纪,并仍在进行中。该地区构造发育,为各种矿产的分布提供了良好的空间。

The Xinjiang Karakoram Yanshan fold system, tectonic development and the South Asian subcontinent and North Eurasia collision related displacement. The main tectonic period began in the Cretaceous and continued to the third period. The uplift of the mountains began in the late third and is still in progress. The tectonic development of the region provides a good space for the distribution of various minerals.