班公湖-怒江带以北,表现为强烈的造山运动,形成规模巨大的印支造山带。
The movement performs in the form of strong orogeny north of Bangonghu-Nujiang suture, which leads to large-scale Indosinian orogenic belt.
班公湖-怒江带以北,表现为强烈的造山运动,形成规模巨大的印支造山带。
The movement performs in the form of strong orogeny north of Bangonghu-Nujiang suture, which leads to large-scale Indosinian orogenic belt.
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