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Stress and Strain Accumulation Due to a Long Dip-Slip Fault Movement in an Elastic-Layer over a Viscoelastic Half Space Model of the Lithosphere-Asthenosphere System

机译：岩石圈-软流圈系统粘弹性半空间模型上的弹性层中的长倾滑断层运动引起的应力和应变累积

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Sanjay Sen; Subrata Kr. Debnath;
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1. Stress and Strain Accumulation Due to a Long Dip-Slip Fault Movement in an Elastic-Layer over a Viscoelastic Half Space Model of the Lithosphere-Asthenosphere System [J] . Sanjay Sen, Subrata Kr. Debnath International Journal of Geosciences . 2013,第3期

机译：岩石圈-软流圈系统粘弹性半空间模型上的弹性层中的长倾滑断层运动引起的应力和应变累积
2. PATTERN OF STRESS-STRAIN ACCUMULATION DUE TO A LONG DIP-SLIP FAULT MOVEMENT IN A VISCOELASTIC LAYERED MODEL OF THE LITHOSPHERE -ASTHENOSPHERE SYSTEM [J] . S. K. DEBNATH, S. SEN International Journal of Applied Mechanics and Engineering . 2013,第3期

机译：岩石球-弹塑性系统粘弹分层模型中长倾角滑动断层运动引起的应力-应变累积规律
3. Creeping Movement across a Long Strike-Slip Fault in a Half Space of Linear Viscoelastic Material Representing the Lithosphere-Asthenosphere System [J] . Papiya Debnath1, Sanjay Sen2 Frontiers in Science . 2014,第2期

机译：在代表岩石圈-软流圈系统的线性粘弹性材料的半空间中，跨越长走滑断层的蠕变运动
4. Love Wave Propagation in an Anisotropic Viscoelastic Layer Over an Initially Stressed Inhomogeneous Half-Space [C] . Bishwanath Prasad, Prakash Chandra Pal, Santimoy Kundu International Conference on Vibration Problems . 2021

机译：在最初强调的非均匀半空间上的各向异性粘弹性层中的热波传播
5. Crustal deformation due to a dipping fault in an elastic gravitational layer overlying a viscoelastic gravitational half space: Models and applications [D] . Yu, Ting-To 1995

机译：覆盖在粘弹性引力半空间上的弹性引力层中的浸渍断层引起的地壳变形：模型和应用
6. Limitations of Viscoelastic Constitutive Models for Carbon-Black Reinforced Rubber in Medium Dynamic Strains and Medium Strain Rates [O] . Francesca Carleo, Ettore Barbieri, Roly Whear, 2018

机译：中等动态应变和中等应变速率下炭黑增强橡胶的粘弹性本构模型的局限性
7. Pattern of Stress-Strain Accumulation due to a Long Dipslip Fault Movement in a Viscoelastic Layered Model of The Lithosphere–Asthenosphere System [O] . S.K. Debnath, S. Sen 2013

机译：由于岩石圈岩石圈系统粘弹性分层模型中的长倾斜式故障运动引起的应力 - 应变累积模式

Stress and Strain Accumulation Due to a Long Dip-Slip Fault Movement in an Elastic-Layer over a Viscoelastic Half Space Model of the Lithosphere-Asthenosphere System

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