Abstract：Altun fault system is a very important major strike-slip fault in Northwest of China.It had undergone several times of clockwise transtensional and counter transpressional movement in geological history.The tectonic style and evolution of Center Tarim area,which is Located in northwest side of Altun fault system,has been influenced intensely by the activity of tlltun fault since Palaeozoic.Its style was formed because of the left-lateral transpression of Altun fault in early of late Caledonian,and its reformation resulted from the left-lateral transpression in early Variscan.
康南昌. 阿尔金断裂系与塔中构造带的形成与演化[J]. 石油地球物理勘探, 2002, 37(1): 48-52.
Kang Nanchang. Altun fault system and formation and evolution of Tazhong structural bell. OGP, 2002, 37(1): 48-52.
