碰撞带 [地质] collision zone
- 地幔流动对地表板块运动、海洋中脊和中隆、俯冲带和碰撞带的分布起着控制作用。
The mantle flow controls the plate movement and the distribution of ocean ridges, subduction zones, and collision zones. - 中国大陆碰撞带是以结构复杂、形成过程复杂和物质成分趋于混杂为主要特征的。
The collision zones in China Continent are mainly characterized by complex structures, complex forming processes and mixed materials. - 近80年来,由喜马拉雅板缘碰撞带向我国大陆板内强震区强震群体活动呈现时空的有序迁移。
In the past 80 years, the groups displayed an ordered space-time migration from Himalayan plate boundary collision zone to the intraplate seismic zones of China's continent.
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