地应力状态与构造断层的相互作用：评论

李鹏; 蔡美峰; Mostafa Gorjian; 任奋华; 席迅; 王培涛

doi:10.1007/s12613-023-2607-8

Volume 30 Issue 7

Jul. 2023

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文章导航 > 矿物冶金与材料学报（英文） > 2023 > 30(7): 1227-1243

Peng Li, Meifeng Cai, Mostafa Gorjian, Fenhua Ren, Xun Xi, and Peitao Wang, Interaction between in situ stress states and tectonic faults: A comment, Int. J. Miner. Metall. Mater., 30(2023), No. 7, pp. 1227-1243. https://doi.org/10.1007/s12613-023-2607-8

Cite this article as:

Peng Li, Meifeng Cai, Mostafa Gorjian, Fenhua Ren, Xun Xi, and Peitao Wang, Interaction between in situ stress states and tectonic faults: A comment, Int. J. Miner. Metall. Mater., 30(2023), No. 7, pp. 1227-1243. https://doi.org/10.1007/s12613-023-2607-8

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地应力状态与构造断层的相互作用：评论

1)
北京科技大学城市地下空间工程北京市重点实验室, 北京 100083, 中国
2)
北京科技大学金属矿山高效开采与安全教育部重点实验室, 北京 100083, 中国
3)
Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia, Vancouver, BC, Canada

通讯作者:
席迅 E-mail: xixun@ustb.edu.cn

王培涛 E-mail: wangpeitao@ustb.edu.cn

文章亮点

(1) 系统地分析了断层附近地应力大小和方向的变异性规律。

(2) 阐明了地应力状态变化对断层活化的影响机制。

(3) 揭示了地应力与断层性质之间的相关性。

中文摘要

在许多工程问题和地球科学研究中，了解地应力状态至关重要。本文旨在系统评述地应力状态与构造断层之间的相互作用，并对它们之间的相互作用机制提出了新的见解。地应力状态会受到各种因素的影响，其中最重要的因素之一是断层的存在。断层会显著影响地应力的大小和方向。在断层附近存在应力的重新定向和大小变化，并且跨断层存在应力跳跃/不连续。反之，应力状态的变化可能导致断层类型的转变和潜在的断层活化。利用当前应力环境下的特征参数对断层活化进行定性评价，提供了一种评价断层滑动趋势的方法。地应力和断层性质之间的相关性增强了通过地应力测量预测断层滑动趋势的能力，这可用于进一步完善断层活化风险的评估。未来在深部进行地应力测量，并在断层的关键部位上/附近进行长期连续的实时应力监测将是必不可少的。此外，需要重点关注区分异常应力状态形成机制和应力变化的类型和规模，探索断层活动前异常和断层活化机制。

关键词:

Invited Review

Interaction between in situ stress states and tectonic faults: A comment

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Abstract

Abstract

Understanding the in situ stress state is crucial in many engineering problems and earth science research. The present article presents new insights into the interaction mechanism between the stress state and faults. In situ stresses can be influenced by various factors, one of the most important being the existence of faults. A fault could significantly affect the value and direction of the stress components. Reorientation and magnitude changes in stresses exist adjacent to faults and stress jumps/discontinuities across the fault. By contrast, the change in the stress state may lead to the transformation of faulting type and potential fault reactivation. Qualitative fault reactivation assessment using characteristic parameters under the current stress environment provides a method to assess the slip tendency of faults. The correlation between in situ stresses and fault properties enhances the ability to predict the fault slip tendency via stress measurements, which can be used to further refine the assessment of the fault reactivation risk. In the future, stress measurements at greater depths and long-term continuous real-time stress monitoring near/on key parts of faults will be essential. In addition, much attention needs to be paid to distinguishing the genetic mechanisms of abnormal stress states and the type and scale of stress variations and exploring the mechanisms of pre-faulting anomaly and fault reactivation.
- in situ stress state;
- stress variation;
- fault reactivation;
- fault properties;
- interaction mechanism

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