The kinematics of Gangou ophiolitic mélange is consistent with that of Kekesu HP metamorphic rocks.
干沟-米什沟蛇绿混杂岩带的变形运动学与科克苏高压变质岩带变形特征完全一致。
2
The newly discovered Karamay ophiolitic mélange distributed along the NW edge of the Junggar basin has a complete sequence of ophiolite and accretionary complex.
新发现的克拉玛依蛇绿混杂岩带分布于准噶尔盆地西北缘，表现为组分齐全的蛇绿岩和增生杂岩。
3
The intrusive bodies are output in stocks, dikes and tectonic slices, which were suffered from later tectonism and evolved in the Kuhai-Saishitang Hercynian mélange belt as tectonic slices.