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笔者总结了西昆仑—帕米尔造山带及塔西南前陆盆地板内变形的各类构造模式、构造分带、新生代变形格局及构造演化,提出其新生代板内变形具有弧形构造分段性和阶段性演化的特点,发现了依格孜牙、柯克亚、桑株—杜瓦、卡兹克—阿尔特薄皮弧形推覆构造、齐姆根主弧形构造段及玉力群—克里阳构造段的三角带构造及叶尔羌—棋盘对冲过渡型弧形构造。认为对冲过渡型弧形构造及各弧形构造分段间的斜冲走滑带是塔西南前陆盆地板内变形的特殊产物。
The authors summarize various types of tectonic modes, structural zoning and Cenozoic deformation patterns and tectonic evolution of the West Kunlun-Pamir orogenic belt and the southwestern Tarim Basin, and propose that the Cenozoic intraplate deformation has arcuate tectonic segments Sex and stage evolution, we found the thin arc-shaped nappe structures of Engezi, Kekeya, Sang Zhu-Dewar, Katsik-Alte, the main arcuate tectonic segment of Zimgen, VERTICAL STRUCTURE OF THE KRIYANG STRUCTURAL SECTION AND YELIANG QIANG - HUSBAND HINGE TRANSITIONAL ARC STRUCTURE. It is considered that the hedge transitional arc structure and the diagonal strike-slip zone between each arc structure segment are the special products of intraplate deformation in the southwestern Tarim basin.