Figure 1: Comparison of earthquake slip determined from surface geodetic displacements with long-term interseismic coupling. Figure 2: Deformation patterns observed in Sentinel-1 interferograms for ...
\(x\) is 50°. Corresponding angles are equal. \(y\) is 180° - 50° = 130°. Angles on a straight line add up to 180°.
一些您可能无法访问的结果已被隐去。
显示无法访问的结果
反馈