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The two-dimensional thermoelastic model of Carpathian region on the basis of a numerical finite elements method is constructed. The physical and mathematical model is as much as possible approached to the real environment. Detailed high-precision distribution of thermoelastic stresses and dislocations is received. The mountainous rocks non-uniform heating and structural non-uniforms leads to considerable changes of stress fields and dislocations in Carpathian region.
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Natalia Bakhova (2010) studied this question.
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