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现代矿业 ›› 2025, Vol. 41 ›› Issue (10): 132-138.

• 地质·测量 • 上一篇    下一篇

闽西煤矿区地质构造基本特征及演化分析

邱占林1,2 郭 鑫1 曾东富3 王占谠4 覃 琼4 赖景祥4 曾桂玲1,2 宋柏霖2   

  1. 1. 龙岩学院资源工程学院;2. 福建水利电力职业技术学院;3. 福建紫金铜业有限公司; 4. 武平县天盛矿业投资集团有限公司
  • 出版日期:2025-10-25 发布日期:2025-12-04

Analysis on the Basic Characteristics and Evolution of Geological Structures in Coal Mining Area of Western Fujian

  1. 1. School of Resource Engineering,Longyan University; 2. Fujian Polytechnic of Water Conservancy and Electric Power;3. Fujian Zijin Copper Co.,Ltd.; 4. Wuping County Tiansheng Mining Investment Group Co.,Ltd.
  • Online:2025-10-25 Published:2025-12-04

摘要: 为查明闽西煤矿区地质构造的基本情况,通过分析其所处的区域构造背景,并结合生 产实际揭露的工程资料,采用构造分析法对闽西煤矿区褶皱、(缓)断裂、准同生构造等地质构造基本 特征进行了统计和初步总结。在此基础上,对其构造应力场以及形成演化模式进行了初步研究。结 果显示:矿区内近EW向构造叠加以及早期EW向构造改造使区域构造更趋于复杂化;区内典型构造 总体上属于下滑上推式、上滑下推式或又滑又推式叠加型构造。褶皱构造主要为近NE和NWW向, 与区域主要大地构造的展布方向基本吻合;断层构造以走向断层和高角度断层为主,与区域构造应 力场的主应力方向基本一致,且经历了印支晚期、燕山早—晚期、喜山晚期等多期次主要构造变动, 并对应于滑覆构造、逆冲推覆型或推滑型边界断裂、控煤构造的形成演化。而且,燕山期岩浆活动对 逆冲推覆构造等矿区总体构造轮廓的产生具有决定性意义。该研究可为今后在类似构造特征发育 地区寻找隐伏煤炭资源以及煤矿顶板安全管理等提供一定的理论参考与借鉴。

关键词: 闽西煤矿区, 地质构造, 构造特征, 演化模式, 构造体系

Abstract: In order to clarify the basic situation of geological structures in coal mining area of western Fujian,by analyzing the regional tectonic background where it is located and combining the engineering da⁃ ta exposed in production practice,the basic characteristics of geological structures such as folds,(gentle) faults and quasi-contemporaneous structures in coal mining area of western Fujian,were statistically ana⁃ lyzed and preliminarily summarized by using the tectonic analysis method. On this basis,the tectonic stress field and evolution model of the area were preliminarily studied. The results show that the superposition of the near EW trending structures and the early EW trending structural reconstruction make the regional struc⁃ tures more complicated. The typical structures in the area generally belong to the superposition type of down⁃ ward sliding and upward pushing,upward sliding and downward pushing,or both sliding and pushing. The fold structures are mainly oriented in the near NE and NWW directions,which are basically consistent with the distribution direction of the main regional geological structures. The fault structures are mainly strike�slip faults and high-angle faults,which are basically consistent with the main stress directions of the region⁃ al tectonic stress field,they have undergone multiple major tectonic changes such as the late Indosinian pe⁃riod,early to late Yanshan period,and late Himalayan period,and correspond to the formation and evolu⁃ tion of the sliding cover structure,thrust nappe or thrust-slip type boundary faults,and coal-controlling structures. Moreover,the magmatic activity of the Yanshan period played a decisive role in the formation of the overall structural profile such as the thrust nappe structure. This study can provide some theoretical refer⁃ ence for searching hidden coal resources and safety management of coal mine roof or other aspects in areas with similar structural characteristics in the future.

Key words: coal mining area of western Fujian, geological structure, structural characteristics, evolu? tion model, tectonic system