关金锋,周侃,司中应,等. 地质因素对松河煤矿瓦斯赋存的控制作用[J]. 中国矿业,2024,33(1):179-185. DOI: 10.12075/j.issn.1004-4051.20230529
    引用本文: 关金锋,周侃,司中应,等. 地质因素对松河煤矿瓦斯赋存的控制作用[J]. 中国矿业,2024,33(1):179-185. DOI: 10.12075/j.issn.1004-4051.20230529
    GUAN Jinfeng,ZHOU Kan,SI Zhongying,et al. Control of geological factors on gas occurrence in Songhe Coal Mine[J]. China Mining Magazine,2024,33(1):179-185. DOI: 10.12075/j.issn.1004-4051.20230529
    Citation: GUAN Jinfeng,ZHOU Kan,SI Zhongying,et al. Control of geological factors on gas occurrence in Songhe Coal Mine[J]. China Mining Magazine,2024,33(1):179-185. DOI: 10.12075/j.issn.1004-4051.20230529

    地质因素对松河煤矿瓦斯赋存的控制作用

    Control of geological factors on gas occurrence in Songhe Coal Mine

    • 摘要: 掌握煤层瓦斯赋存特征可为煤层气资源开发和煤矿瓦斯灾害治理提供理论指导,煤层瓦斯赋存受地质因素所控制,为揭示地质因素对松河煤矿瓦斯赋存的控制作用,采用地质统计法、构造控制理论,结合矿区大地构造位置、构造演化和区域构造应力场的特点,分析了矿区构造、矿井构造、小型构造的特征,探讨了其对瓦斯赋存的控制作用。结果表明:盘江矿区煤层主要受燕山运动和喜马拉雅运动影响,海陆交替相沉积环境、构造抬升和后期风化剥蚀作用,导致背斜煤层风化剥蚀、向斜煤层当中瓦斯得以保存,煤层瓦斯由向斜两翼向核部逐渐增大。“三角形弧系”构造应力场控制矿区构造变形及构造煤发育,在“三角形弧系”构造的顶角位置的构造变形强烈、煤体变形严重,煤层瓦斯含量相对较高,而在“三角形弧系”构造的边部构造变形弱、构造煤发育程度低,煤层瓦斯含量相对较低。松河煤矿位于“三角形弧系”构造边部的土城向N翼弱构造变形区,致使煤层整体上受构造破坏作用小,构造煤发育程度低,在煤层局部范围发育有压性或压扭性断裂,煤层埋深是松河煤矿煤层瓦斯赋存的主控因素,而压性或压扭性断裂附近是瓦斯灾害局部防治的重点,对松河煤矿以及具有相似地质条件的煤矿实施精准瓦斯治理工作具有指导意义。

       

      Abstract: Mastering the characteristics of coal seam gas occurrence can provide theoretical guidance for coal seam gas resource development and gas disaster control. In order to reveal the controlling geological factors on the gas occurrence in Songhe Coal Mine, the characteristics of structure of mine area, mine structure and small structure are analyzed by geological statistics method and structure control theory, combined with the characteristics of tectonic location, tectonic evolution and regional tectonic stress field, and their controlling effect on gas occurrence is discussed. The results show that the coal seam of Panjiang Mining Area is mainly affected by Yanshan Tectonic and Himalayan Movement, the sedimentary environment of alternating marine facies, tectonic uplift and weathering denudation in the later period lead to weathering denudation of anticlinal coal seam and preservation of gas in synclinal coal seam, and the gas in coal seam increases gradually from the synclinal flank to the core. The “triangle arc system” tectonic stress field controls the tectonic deformation and tectonic coal development in the mining area. The top corner of the “triangle arc system” structure has strong tectonic deformation and serious coal deformation, and the gas content is relatively high, while the side of the “triangle arc system” structure has weak tectonic deformation and less tectonic coal, and the gas content is relatively low. Songhe Coal Mine is located in weak tectonic deformation area of the Tucheng-N-wing on the edge of the “triangle arc system” structure, resulting in little tectonic damage to the coal seam, low degree of tectonic coal development as a whole, only compression or compression-torsion fracture developed in local coal seam. It is determined that the buried depth of coal seam is the main control factor of gas occurrence in Songhe Coal Mine. The area near compressive or compressive torsion fracture is the focus of local gas disaster control. It is of guiding significance for Songhe Coal Mine and other coal mines with similar geological conditions to implement accurate gas control.

       

    /

    返回文章
    返回