Kümüx

From the evidence of the latest Ludlovian to Early Devonian ophiolite, which crops out from the northern slope of Mt. Saarming to Kümüx and areas further east (Wang Zuoxun et al., 1986, 1990; Xiao Xuchang et al., 1990), the South Tianshan back-arc basin had already developed into a finite ocean basin along the Hantengri-Kümüx Fault after the Ludlovian.