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Quasi-static Planar Deformation in a Medium Composed of Elastic and Thermoelastic Solid Half Spaces Due to Seismic Sources in an Elastic Solid

机译：由于弹性固体中的震源，在由弹性和热弹性固体半空间组成的介质中的准静态平面变形

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Anil K. Vashisth; Kavita Rani; Kuldip Singh;
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1. 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
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 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
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] . Sarva Jit Singh2, Sunita Rani1 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. Elastic-wave scattering from a solid circular cylinder embedded in an elastic half-space [C] . Lawrence, D.E., Sarabandi, Geoscience and Remote Sensing Symposium, 2002. IGARSS '02. 2002 IEEE International . 2002

机译：来自嵌入弹性半空间的实心圆柱体的弹性波散射
5. Meshless methods in shape optimization of linear elastic and thermoelastic solids. [D] . Bobaru, Florin. 2001

机译：线性弹性和热弹性实体形状优化中的无网格方法。
6. The anelastic Ericksen problem: universal eigenstrains and deformations in compressible isotropic elastic solids [O] . Arash Yavari, Alain Goriely -1

机译：无弹性埃里克森问题：可压缩各向同性弹性固体的普遍本征应变和变形
7. Quasi-static deformation due to two-dimensional seismic sources embedded in an elastic half-space in welded contact with a poroelastic half-space [O] . Sunita Rani, Sarva Jit Singh 2007

机译：由于二维地震源引起的准静态变形，其嵌入焊接接触的弹性半空间中，焊接接触与孔弹性半空间
8. THERMODYNAMICS OF ELASTIC AMD OF SOME V1SC0-ELASTIC SOLIDS AND NON-LINEAR THERMOELASTICITY [R] . Boa-Teh Chu 1957

机译：一些V1sC0-弹性体的弹性amD的热力学和非线性热弹性

Quasi-static Planar Deformation in a Medium Composed of Elastic and Thermoelastic Solid Half Spaces Due to Seismic Sources in an Elastic Solid

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