摘要
过去１０年中，中美、中法地球物理科学家和地质学家曾经在青藏高原进行数次联合观测．本文综述了联合观测中利用垂直地震反射、广角地震反射以及宽频带数字地震仪进行观测的结果，并将它们进行比较．可以得知，青藏高原内部岩石圈构造的横向差异相当重要，这些异常需要进一步加以检验．
In last decade, several international joint projects in Tibetan plateau were conducted by Chinese, American and French geophysicists and geologists. In the present review,the results from vertical reflections, wide-angle reflections and broadband digital seismic recordings are reviewed and compared. Constraints for the dynamics of continent-continent cllision from the lithospheric structures,seismicity, focal mechanism and anisotropy are discussed.
出处
《地球物理学报》
SCIE
EI
CSCD
北大核心
1994年第A02期99-116,共18页
Chinese Journal of Geophysics
基金
国家自然科学基金
关键词
青藏高原
岩石圈构造
动力学
大陆碰撞
Lithospheric structure,Dynamics,Tibetan Plateau, Continental collision.
