Early Cambrian syndepositional structure of the northern Tarim Basin and a discussion of Cambrian subsalt and deep exploration

GUAN Shuwei,ZHANG Chunyu,REN Rong,ZHANG Shuichang,WU Lin,WANG Lei,MA Peiling,HAN Changwei

Fig. 11. Variations of Xiaoerbulake Formation sedimentary structures along the synsedimentary faults at the northern slope of the Tazhong uplift and the southern slope of the Tabei upift (all sections were flattened at the bottom of the Xiaoerbulake Formation, and the locations are shown in Fig. 9).