位置：成果数据库 > 会议 > 会议详情页
The extension of the frequency range of the seismic profile recorded by geophone-TEXAN system
  • 所属机构名称：中国地质大学（武汉）
  • 会议名称：International Workshop on Multiple-scale Geodynamics of Continental Interiors, Wuhan, China
  • 成果类型：会议
  • 会场：武汉
  • 相关项目：长江三峡地区壳幔三维结构与地震活动性研究
作者： 姚运生|邹志辉|周华伟|李强|廖武林|
同会议论文项目
长江三峡地区壳幔三维结构与地震活动性研究
期刊论文 38 会议论文 28
同项目会议论文
Multi-scale layering in crust and upper mantle seismic structures
3D gravity imaging of deep geological structure of Huangling Anticline in Three Gorges area, China
Studying the lithospheric structure and seismotectonics of the Three-Gorges Reservoir region, China
Overcoming uneven ray coverage in crustal seismic tomography of the Three Gorges Reservoir, China
Shallow velocity imaging of mining districts from active source tomography
球坐标系中的卫星重力三维反演方法研究
Co-seismic corresponding analysis of the Earth’s free oscillations gravity signal induced by t
Relocating small earthquakes with reverse time modeling: Examples in the Three Gorges Reservoir regi
2D Tomographic velocity model building in tilted transversely isotropic media
基于球冠的卫星重磁数据处理与分析方法
Mapping seismic velocities beneath the Yangtze Three Gorges Reservoir
Assessing the reliability of low frequencies in geophone records
Tomographic velocity model building of near surface with reversed-velocity interfaces
Reverse time imaging of small earthquakes using 2D array data in Three Gorges Reservoir region
Blind Testing of Deformable Layer Tomography Using Near-Surface First Arrivals
Assessing the reliability of low frequencies in geophone records
Crustal 3D velocity structure beneath the Three Gorges Reservoir
First arrival tomography using depth-varying velocity gradients
A10/022绝对重力仪的性能分析及试验观测结果
基于空间域的GRACE时变重力场去噪方法研究及应用
基于磁异常模量的三维磁化率成像研究及应用
重力梯度张量数据的反演方法研究
Three-dimensional density structure of the lunar upper lithosphere
Preliminary comprehension about satellite gravity and magnetic anomaly distributions in the Philippi
二维经验模态方法在中国及邻区卫星磁异常多尺度分解中的应用
The role of acquisition geometry and components for imaging microseismicity
Improved shortest-path ray tracing with locally linear velocity variations