【摘要】 在对齐姆根弧形构造地表地质构造和深部地球物理资料综合分析的基础上 ,阐述了齐姆根弧形构造的几何学、运动学和分段性 ,提出了齐姆根弧形构造由依格孜牙薄皮推覆构造段、齐姆根主弧形三角带构造段和叶尔羌—棋盘对冲构造段组成 ,各弧形构造段之间以横向走滑—斜冲断层为界 ;发现了齐姆根弧形构造中规模巨大的塔里木西南盆地白垩系—新生界沉积盖层向西昆仑—帕米尔被动反 (逆 )冲逆掩构造系统 ,阐述了齐姆根主弧形构造段由铁克里克主动逆冲推覆系统、塔里木西南盆地被动反冲逆掩系统和深部双重构造组成。齐姆根弧形构造的隆升时期为喜马拉雅运动 ,新生代 ,尤其是第四纪以来西昆仑—帕米尔向北和北东整体推移导致的深部双重构造是齐姆根弧形隆升的主因更多还原

【Abstract】 Based on a comprehensive analysis of the Qimugen arcuate structure in terms of the field geological structures and geophysical data, this paper presents a description of the geometry and kinematics of the Qimugen arcuate structure and suggests that it consists of three segments, i.e. the Yigeziya thin skin nappe structure segment, the Qimugen main arcuate and triangle zone segment and the Yarkant—Qipan ramp structure segment. The segments are bounded by strike slip faults. It is discovered that a huge Cretaceous—Quaternary sedimentary cover of the Southwest Tarim Basin back thrust toward the West Kunlun—Pamir. The main Qimugen arcuate structure is a typical triangle zone which consists of the Tiekelike active thrusting system, the Southwest Tarim Basin passive thrusting system and the deep seated duplex structure. The uplift of the Qimugen arcuate structure took place during the Himalayan orogeny, mainly attributed to the deep duplex structure resulting from the northward or northeastward migration of the West Kunlun—Pamir in the Cenozoic, especially since the Quaternary.更多还原