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- mantle convection hypothesis 地幔对流说
- Cretaceous Large Igneous Provinces and mantle convection. 白垩纪大火成岩省与地幔对流
- The issue of upper vs whole mantle convection is critically discussed. 最后,着重讨论了上地幔与全地幔对流的论争。
- Therefore, the CMB is the beginning and the end of whole mantle convection. 因此,地幔底层既是全地幔对流的起点,又是全地幔对流的终点。
- The rise of the asthenosphere,the position of Moho and mantle plume are the indication of the mantle convection. 软流圈上涌高度、莫霍面或地幔羽的位置是地幔对流的具体的表现。
- The three regions of mantle convection beneath East-Asia and Western-Pacific agree with Western-Pacific, Asia and tethyan tectonic regions. 勾勒出南海地区构造特征:从上到下的大体结构是上部呈“工”字型、中间为圆柱型、底部呈盾形的地幔上升流。
- It is very important to use noncomplete elastic coefficient to study massif stabilitty, earthquake gestation, mantle convection and continent dynamics. 摘要地球介质非完全弹性参数对于研究地体稳定、地震孕育、地幔对流、大陆动力学是非常重要的。
- These interactions may also serve as important ways for lithosphere recycling and mass exchange between the shallow and deep parts of the Earth, which could significantly affect deep mantle convection and surface tectonic processes. 这种相互作用被认为是稳定克拉通岩石圈遭受改造甚至破坏的深部机制,同时还是地球深、浅部物质交换的重要方式,因而显著影响着地球深部的对流和地表的构造过程。
- Small scale of mantle convection restricted in asthenosphere diverges in sea basins, converges in Okinawa Trough and Mariana Trough, and it can be generally analogized with isostatic gravity anomaly. 小尺度地幔流主要限于软流圈层内部 ,在各海盆分散 ,而在冲绳海槽和马里亚纳海槽则会聚 ,可与均衡重力异常类比。
- ADVANCES IN MANTLE CONVECTION STUDY 地幔对流研究的一些新进展
- Progress in mantle dynamics--mantle convection 地幔动力学研究进展--地幔对流
- CORIOLIS FORCE IN MANTLE CONVECTION 地幔对流中的科里奥利力
- A MANTLE CONVECTION MODEL DRIVED BY DENSITY ANOMALIES IN MANTLE 地震层析成像之密度异常驱动地幔对流模型
- All these fact have borne out the hypothesis. 所有这些事实证明了假设的正确性。
- UPPER MANTLE CONVECTION DRIVING BY DENSITY ANOMALY AND A TEST MODEL 上地幔密度异常驱动小尺度对流及实验模型
- Cretaceous Large Igneous Provinces and mantle convection 白垩纪大火成岩省与地幔对流
- Several conclusions flow from this hypothesis. 从这项假设中可以得出几个结论。
- His new hypothesis is considered probable. 他作出的新假设被认为是有充分根据的。
- THE INFLUENCE OF TRENCH RETROGRADATION ON MANTLE CONVECTION 海沟后退对地幔对流的影响
- In convection, hot currents flow upwards. 在对流中热气流向上运动。