该蛇绿混杂岩带是义敦碰撞造山带大地构造相中的弧前混杂带相。
The ophiolite melange zone represents forearc melange facies of the Yidun collision orogens.
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。
The kinematics of Gangou ophiolitic mélange is consistent with that of Kekesu HP metamorphic rocks.
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。
The newly discovered Karamay ophiolitic mélange distributed along the NW edge of the Junggar basin has a complete sequence of ophiolite and accretionary complex.
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