通古斯河和维柳河的应力和应变状态的计算机模拟

IF 0.3 Q4 MECHANICS
A. Akhmetov, I. Smolin
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引用次数: 0

摘要

数值分析了在维柳伊断裂南段和通古斯断裂中段拉张地球动力过程条件下的应力和应变状态。根据深地震测深获得的金伯利特-1981地质剖面,建立了维柳伊联合带南段和通古斯加联合带中段的二维地质构造模型。为了描述几何形状中的塑性应变,采用了基于Drucker-Prager-Nikolaevskii模型的非关联塑性流动规律弹塑性介质模型。该模型采用“果冻三明治”强度模型对岩石圈的应力状态进行分析。本文介绍了西伯利亚克拉通选定部分应力应变状态的数值模拟结果。塑性应变的局部化、水平应力的正值区域以及计算压力与静岩压力的负偏差对应于矿床。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Computer modelling of the state of stress and strain of the Tunguska and Vilyui syneclises
The states of stress and strain are numerically analyzed under conditions of the geodynamic process of tension in the south part of the Vilyui syneclise and the middle part of the Tunguska syneclise. Two-dimensional models of geological structures of the south part of the Vilyui syneclise and the middle part of the Tunguska syneclise are constructed based on the Kimberlit-1981 geological profile obtained using deep seismic sounding. To describe the plastic strain in the geomedia, the model of elastic-plastic media with the non-associated plastic flow rule based on the Drucker-Prager-Nikolaevskii model is used. In this model, the “jelly sandwich” strength model is adopted for the analysis of the stress state of the lithosphere. The results of the numerical modeling of the state of the stress and strain of the chosen parts of the Siberian Craton are presented. The localization of plastic strain, the region of positive values of horizontal stresses, and the negative deviation of the calculated pressure from the lithostatic pressure correspond to mineral deposits.
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来源期刊
CiteScore
0.90
自引率
66.70%
发文量
0
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