The author also examined a frontal tectionic transform domain of Parmir-west kunlun in Qimeigan region, which made it discontinous between the frontal overthrusting belt and the subsiding belt.

• 同时作者还在七美干一带发现帕米尔-西昆仑前缘构造转换域的存在，使得前陆冲断带和前陆沉降带横向不能连接，因而山前的构造变形呈现分阶段发育的特征。