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通过对扎伊尔山至哈拉阿拉特山一带详细的构造变形分析,揭示出准噶尔西北缘主要发育以下3组构造组合:近南北向、北东-南西向和近东西向.其变形序列为:晚石炭世早期,发育近南北向褶皱-冲断构造;晚石炭世时期,近南北向构造线受牵引拖拽呈北东-南西向,达尔布特、克拉玛依蛇绿混杂岩以右旋走滑拉出或侧向楔冲形式构造就位于上覆石炭系中;晚石炭世晚期至二叠纪,发育以达尔布特断裂为代表的北东-南西向伸展断裂,伴随广泛的中基性岩脉及花岗岩侵入;二叠纪末至三叠纪初,发育广泛的近东西向劈理、哈山一带逆冲推覆构造及达尔布特左旋走滑活动.石炭纪至二叠纪,西准地区经历了从俯冲到碰撞再到碰撞后陆内变形的演化过程,伴随着挤压和伸展多期构造叠加,充分体现了该地区复杂构造转换变形的动力学过程.
Through the detailed tectonic deformation analysis from Zaire Mountain to Hala’alat Mountain, it is revealed that the following three tectonic assemblages are mainly developed in the northwestern part of Junggar: near North-South direction, North-East-South West direction and Near East-West direction.The deformation sequence is : Early Late Carboniferous developed nearly south-north fold-thrust structure. During the Late Carboniferous, the NW-NW tectonic line was dragged and dragged northeast-southwest, and the diabite and Karamay ophiolite melanes were dextralized Slippery-out or lateral wedge-shaped structures are located in the overlying Carboniferous. From the late Late Carboniferous to Permian, the NE-SW direction, represented by the Darbat fault, is developed with extensive mesogenic Diagenesis and granite intrusions. During the Late Permian to Early Triassic, there were extensive near-east-west cleavage, thrust-nappe structure and Darbot left-lateral strike-slip activity in the area of Hassan. From Carboniferous to Permian, west The quasi-regional experienced the evolution of the intracontinental deformation from subduction to collision and then collision. With the superimposition of multiple stages of extrusion and extension, the dynamic process of complex structural transformation and deformation in the area was fully demonstrated.