仁布蛇绿构造混杂带位于雅鲁藏布江缝合带中段之最东部，其间混杂伴生有大量较为新鲜的辉绿岩构造岩块。
The Renbu ophiolitic mélange zone locates in the easternmost middle section of the Yarlung Zangbo suture zone, and there are lots of fresh diabase tectonic block outcrops in the mélange zone.
凯蒙蛇绿岩的确定表明嘉黎断裂在早期（T_3-J_1）可能是冈底斯构造带上的一条重要缝合带。
The definition of Kaimeng ophiolite shows that Jiali fault may be an important suture in Gangdese tectonic belt during T_3 -J_1.
在昆仑山脉与雅鲁藏布缝合带之间，向东的流动便形成上部地壳的滑脱构造。
Between the Kunlun fault and Yarlung Zangbo suture the eastward flow resulted in the formation of detachments in the upper crust.
应用推荐