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ORIGINAL RESEARCH article

Front. Earth Sci.

Sec. Geohazards and Georisks

Volume 13 - 2025 | doi: 10.3389/feart.2025.1556612

Study on the mechanism of mining-induced seismicity triggered by fracture of hard and extremely thick rock stratum: a case study

Provisionally accepted
Jinrong Cao Jinrong Cao 1*Linming Dou Linming Dou 1*Xiufeng Zhang Xiufeng Zhang 2Siyuan Gong Siyuan Gong 1Yueyong Han Yueyong Han 2Guoying Li Guoying Li 2Chuancheng Liu Chuancheng Liu 3Yang Chen Yang Chen 2
  • 1 China University of Mining and Technology, Xuzhou, China
  • 2 Coal Industry Management Department, Shandong Energy Group Co., Ltd, Jinan, Shandong, China
  • 3 Shandong Energy Group Technology Development Co., Ltd, Jinan, Shandong, China

The final, formatted version of the article will be published soon.

    The control of mining-induced seismicity caused by hard and extremely thick rock stratum (HETRS) has become an important topic in more and more coal mines. This study investigates the mechanisms of mining-induced seismicity through a discrete element numerical model (UDEC-Trigon) calibrated with field data from the Dongtan Coal Mine, China. The failure process of HETRS was categorized into three stages: deformation (Stage I), initial fracture (Stage II), and periodic fracture (Stage III). In the initial fracture stage, the change of vertical displacement is 4.33 m, the change of vertical stress is 26.21 MPa, and the change of seismic energy is 1.91E8 J. The change values during the initial fracture are the largest. A novel method was developed to dynamically track seismic events, identifying tensile failures in central HETRS and shear failures along interfaces. The total decrement of gravitational potential energy is 2.27E10J. The total increment of shear dissipation energy, plastic strain energy and mining-induced seismic energy are 1.16E9J, 1.49E9J and 2.84E10J. Therefore, in addition to elastic energy, gravitational potential energy is also the main source of mining-induced seismic energy and dissipation energy. The mining-induced seismicity energy comes from the fractured strata as well as the surrounding rock. The results provide a unique perspective to understand the mechanism of mining-induced seismicity triggered by HETRS.

    Keywords: Hard and extremely thick rock stratum, Stress evolution, Crack development, Energy transformation, Mining-induced seismicity

    Received: 07 Jan 2025; Accepted: 10 Mar 2025.

    Copyright: © 2025 Cao, Dou, Zhang, Gong, Han, Li, Liu and Chen. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

    * Correspondence:
    Jinrong Cao, China University of Mining and Technology, Xuzhou, China
    Linming Dou, China University of Mining and Technology, Xuzhou, China

    Disclaimer: All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article or claim that may be made by its manufacturer is not guaranteed or endorsed by the publisher.

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