Origin and growth mechanisms of strike-slip faults in the central Tarim cratonic basin, NW China

WU Guanghui,MA Bingshan,HAN Jianfa,GUAN Baozhu,CHEN Xin,YANG Peng,XIE Zhou

Fig. 8. The structural topograph of the top of the Orovician carbonate at the end of the Middle Ordovician in Tarim Basin (a) and rose diagram of strikes of conjugate faults and the principal stress direction in Halahatang area, northern Tarim (b) (modified after reference [35]).