欢迎您！东篱公司
退出
-
申报数据库
-
立项数据库
-
成果数据库
-
项目获奖数据库
中文摘要：
地球内核缓慢结晶于高度均匀的液态外核，长期被视为简单的均质铁镍合金球体。然而，近年的地震观测揭示了内核各尺度不均匀结构的存在。其中大到（约1000km）全球尺度的准东西半球分划，
同期刊论文项目
同项目期刊论文
Intermediate-depth earthquakes beneath the Pamir-Hindu Kush Region: Evidence for collision between t
Mantle flow pattern and geodynamic cause of the North China Craton reactivation: Evidence from seism
Concordant structural variations from the surface to the base of the upper mantle in the North China
Crustal thickness and Vp/Vs ratio of the central and western North China Craton and its tectonic imp
Seismic evidence for significant lateral variations in lithospheric thickness beneath the central an
Discontinuity structure of the mantle transition zone beneath the North China Craton from receiver f
Lithospheric structure variations between the eastern and central North China Craton from S- and P-r
Structure of the crust and uppermost mantle of the Yanshan Belt and adjacent regions at the northeas
Distinct variations of crustal shear wave velocity structure and radial anisotropy beneath the North
Local modification of the lithosphere beneath the central and western North China Craton: 3-D constr
期刊信息
位置：