• 责任者：Liu Xiaohuang (No.7 Gold Detachment ; CAPF ; Yantai 264004 ; China) ; Niu Shuyin
• 刊名：Northwestern Geology
• 出版年：2013
• 卷期：46(4)
• 关键词：古生代 ; Paleozoic ; 不整合 ; unconformities ; 新疆 ; Xinjiang
• 页码：p.115-130
• 图表：7 illus., 2 tables, 152 refs.
• 分类号：1200
• issnNo：ISSN1009-6248
• isbnNo：CN61-1149/P

     Halaqi region is located in Southwest Tianshan-Northwest Tarim Basin. It＇s the front region of collision between Tarim Block and Kazakhstan-Siberia Block. Cambrian-Permian strata with slight metamorphism outcropped in this area, where we discover three unconformity surfaces, namely angular unconformity in Permian-Cenozoic, parallel unconformity in Ordovician-Silurian and parallel unconformity in Devonian-Carboniferous. The unconformity is bordered by Aferpaqueyiqieke vault anticlinorium. The sedimentary environment on both sides of Silurian-Permian is greatly different. The metamorphism in Ordovieian and Cambrian composed of anticline is different from that of overlying strata. According to regional geology and evolution,the parallel unconformity in Ordovician-Silurian was corresponding to the regional Qilian Movement. The parallel unconformity in Devonian-Carboniferous was corresponding to the middle Tianshan Movement. The angular unconformity in Permian-Cenozoic was influenced by the end of Tianshan Movement.