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Static deformation due to two-dimensional seismic sources embedded in an isotropic half-space in smooth contact with an orthotropic half-space

机译：由于双层半空间中的二维地震源引起的静态变形，其与正向半空间平稳接触

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Yogita Godara; Ravinder Kumar Sahrawat; Mahabir Singh;
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1. Static deformation due to two-dimensional seismic sources embedded in an isotropic half-space in smooth contact with an orthotropic half-space [J] . Yogita Godara, Ravinder Kumar Sahrawat, Mahabir Singh Global Journal of Mathematical Analysis . 2014,第3期

机译：二维地震源嵌入各向同性半空间并与正交异性半空间平滑接触而引起的静态变形
2. Quasi-static deformation due to two-dimensional seismic sources embedded in an elastic half-space in welded contact with a poroelastic half-space [J] . Sunita Rani, Sarva Jit Singh Proceedings of the Indian Academy of Sciences. Earth and Planetary Sciences . 2007,第2期

机译：埋入在弹性半空间中的二维地震源与多孔弹性半空间的焊接接触导致的准静态变形
3. Quasi-static deformation due to two-dimensional seismic sources embedded in an elastic half-space in welded contact with a poroelastic half-space [J] . Sunita Rani, Sarva Jit Singh Journal of Earth System Science . 2007,第2期

机译：埋入在弹性半空间中的二维地震源与多孔弹性半空间的焊接接触导致的准静态变形
4. Mathematical Modeling of G type Seismic Waves in a Homogeneous Layer over a Transversely Isotropic Half-space under Initial Stress [C] . Santimoy Kundu, Shishir Gupta, A. Chattopadhyay, World Congress on Engineering . 2012

机译：在初始应力下横向各向同性半空间在均匀层中G型地震波的数学建模
5. Numerical evaluation of harmonic Green's functions for general anisotropic half-space with embedded sources. [D] . Chen, Zhengxiang. 2005

机译：具有嵌入源的一般各向异性半空间谐波格林函数的数值评估。
6. Influence of tangential displacement on the adhesion strength of a contact between a parabolic profile and an elastic half-space [O] . Valentin L. Popov, Iakov A. Lyashenko, Alexander E. Filippov 2017

机译：切向位移对抛物线轮廓与弹性半空间接触的附着强度的影响
7. Static Deformation due to Two-Dimensional Seismic Sources Embedded in an Isotropic Half-Space in Welded Contact with an Orthotropic Half-Space. [O] . Sarva Jit Singh, Sunita Rani 1991

机译：由于二维地震来源引起的静态变形，其在焊接接触中的各向同性半空间中与正反的半空间中的各向同性半空间。

Static deformation due to two-dimensional seismic sources embedded in an isotropic half-space in smooth contact with an orthotropic half-space

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