贝尼奥夫带

  • 网络Benioff zone;H.Benioff
贝尼奥夫带贝尼奥夫带
  1. 当这些物质熔融形成岩浆,从贝尼奥夫带喷发时,这些物质将发生长期的再循环。

    Long-term recycling of these materials will occur when they are melted to form magmas erupted from the Benioff zone .

  2. 深度在200公里至500公里之间,主压应力方向近于水平,并与贝尼奥夫带走向垂直,张应力轴相对集中。

    In the region of depth from 200 km to 500 km . the most of P axes are nearly horizontal and perpendicular to the strike direction of the Benioff zone ;

  3. 贝尼奥夫带的地震都分布在下降岩石圈板块内。

    Earthquakes along Benioff zones are distributed in the descending lithosphere slabs .

  4. 那边,在那空地里,有一块石板,我正躺下去.贝尼奥夫带的地震都分布在下降岩石圈板块内。

    Yonder , in the square , I meant to sleep on a stone bench . Earthquakes along Benioff zones are distributed in the descending lithosphere slabs .