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研究区位于锡林浩特市北东约40公里处,按照传统的大地构造理论,隶属于天山—兴蒙地槽系,二级构造单元位于兴安地槽南缘。处于二连——贺根山断裂以南及西拉木伦断裂以北之间,并在大兴安岭主脊——林西断裂之西侧的锡林浩物微板块北缘,且是新生代盆地中两个岛状山地之一,面积约
The study area is located about 40 kilometers to the north east of Xilinhot. According to the traditional theory of tectonics, the study area belongs to the Tianshan-Xingmei Trench System, and the secondary structural units are located on the southern margin of Xingan Trough. Located between the Erlian-Hegen Shan fault and the north of the Xilulunru fault and on the northern edge of the Xilin Holocene Microfacies on the west side of the main ridge-Linxi Fault in the Greater Xing’an Mountains, One of two island-shaped mountains with an area of about