不近人情 发表于 2025-3-28 18:08:36
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Stress, Strain, and Elasticity,initesimal strain tensor, more general strain tensors are introduced from displacement field gradients in preparation for finite deformation study. Anisotropic elasticity is discussed with elastic stiffness and elastic compliance expressed both in the standard Vogit matrix notation and in terms of f前奏曲 发表于 2025-3-29 10:28:36
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Flow and Finite Deformation in Tabular Zones,n discuss the finite strain geometry in homogeneous zones with parallel boundaries (tabular zones). There is a rich literature on the kinematic modeling of high-strain zones since Ramsay and Graham (.). We review and summarize the work in a unified approach in this Chapter. Geologists commonly regar可忽略 发表于 2025-3-29 23:17:08
Constitutive Equations,responses in this Chapter. The mathematical relations between the strain or strain rate tensor and the stress tensor for material are called, variably, the constitutive equations, rheological equations, or flow laws. In addition to the elastic behavior, other rheological behaviors such as viscous, pRange-Of-Motion 发表于 2025-3-30 00:34:03
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