Preliminary field investigation of the Zhanda basin in the Ngari area, Tibet, indicate that not only the boundary fault is very active but also many active faults are newly found in the basin, and in addition, there are voluminous olistostromes.
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美
- 摘要野外初步調查結果表明,札達盆地不僅邊界斷裂存在較強烈的活動(dòng)性,而且在盆地內部發(fā)現了較多的活動(dòng)斷層,同時(shí)還伴有大量的崩塌堆積。