新疆阿合奇县位于西南天山与塔里木盆地西北缘的过渡地带,是古亚洲洋和古塔里木地台古生代陆缘造山带的重要组成部分。南部受向南逆冲的喀拉俊—柯坪塔格弧形推覆构造系统控制;北部受大型左旋压扭性迈丹—喀拉铁克断裂带控制。该区由于其特殊的地理位置而受到长期的构造影响,自20世纪以来一直被地质学家所关注。早在20世纪初,一些国外地质 The Xinjiang Autonomous Region, located in the transitional zone between the southwest Tianshan Mountains and the northwestern margin of the Tarim Basin, is an important part of the Paleozoic marginal orogenic belt of the ancient Asian and ancient Tarim platforms. The southern part is controlled by a southward thrusting Khalajun-Kepingtag arcuate nappe structure system; the north is controlled by a large-scale left-lateral compressive Maidan-Karazak fault zone. The area is influenced by long-term tectonics due to its special geographical location and has been the focus of geologists since the 20th century. As early as the early 20th century, some foreign geology