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淮北煤田钱营孜矿井控煤构造特征及其动力学背景分析

汪伟民 顾承串 程龙艺 吴基文 翟晓荣

汪伟民, 顾承串, 程龙艺, 吴基文, 翟晓荣. 淮北煤田钱营孜矿井控煤构造特征及其动力学背景分析[J]. 地质科技通报, 2024, 43(3): 133-146. doi: 10.19509/j.cnki.dzkq.tb20230436
引用本文: 汪伟民, 顾承串, 程龙艺, 吴基文, 翟晓荣. 淮北煤田钱营孜矿井控煤构造特征及其动力学背景分析[J]. 地质科技通报, 2024, 43(3): 133-146. doi: 10.19509/j.cnki.dzkq.tb20230436
WANG Weimin, GU Chengchuan, CHENG Longyi, WU Jiwen, ZHAI Xiaorong. Characteristics and geodynamic background of the coal-controlled structural patterns in the Qianyingzi Coalmine, Huaibei Coalfield[J]. Bulletin of Geological Science and Technology, 2024, 43(3): 133-146. doi: 10.19509/j.cnki.dzkq.tb20230436
Citation: WANG Weimin, GU Chengchuan, CHENG Longyi, WU Jiwen, ZHAI Xiaorong. Characteristics and geodynamic background of the coal-controlled structural patterns in the Qianyingzi Coalmine, Huaibei Coalfield[J]. Bulletin of Geological Science and Technology, 2024, 43(3): 133-146. doi: 10.19509/j.cnki.dzkq.tb20230436

淮北煤田钱营孜矿井控煤构造特征及其动力学背景分析

doi: 10.19509/j.cnki.dzkq.tb20230436
基金项目: 

国家自然科学基金青年基金项目 41902212

安徽恒源煤电股份有限公司2021年科研计划项目"钱营孜煤矿西一东一间孤立块段构造发育规律研究" 

详细信息
    作者简介:

    汪伟民, E-mail: 45133264@qq.com

    通讯作者:

    顾承串, E-mail: guchengchuan15@163.com

  • 中图分类号: P618.11

Characteristics and geodynamic background of the coal-controlled structural patterns in the Qianyingzi Coalmine, Huaibei Coalfield

More Information
  • 摘要:

    钱营孜矿井位于淮北煤田宿县矿区的西部, 毗邻徐宿弧形推覆构造南段的外缘带。为认识该矿井构造变形与演化规律、动力学机制以及指导未来资源探采方向提供重要地质依据。利用最新的矿井地质勘探与生产资料, 对钱营孜矿井开展构造格架和控煤构造样式分析, 划分矿井构造期次, 讨论构造发育的区域大地构造背景。结果表明, 矿井内石炭纪-二叠纪含煤地层总体呈一轴向NNE、向SSW仰起的宽缓向斜; 矿井内断裂构造非常发育, 逆断层数量大于正断层, 2类断层的走向均以NE至NNE向为主, 其次为NS向; 矿井构造格架显著受控于数条NS向至NE向的大型断层, 自西向东受南坪断层、F22、F17、DF200及双堆断层等主干断层的分割, 呈现东、西分带特征; 矿井控煤构造样式可以划分为挤压、伸展和走滑3个类型, 以及逆冲牵引褶皱、对冲式构造、冲起构造、叠瓦状构造、地堑、地垒、阶梯状断层、正花状构造、羽状雁列式构造9个亚类型; 构造组合分析表明, F17断层除逆冲活动之外, 还存在显著的平移活动。矿井构造可划分为5期, 从早到晚分别为: 轴向NNE的冯家向斜、近NS向逆断层、NNE向逆-左行平移断层及NE向逆断层、近NS向正断层、NE向正断层。矿井内第1, 2期缩短构造分别是印支期华北克拉通与华南板块汇聚过程中的前陆变形及随后陆-陆碰撞造山变形的影响结果; 第3期压扭性构造与西太平洋区伊泽奈崎板块早白垩世初向东亚大陆边缘快速斜向俯冲有关; 第4, 5期伸展构造则是早白垩世以来中国东部强烈伸展背景下发育而成。

     

  • 图 1  华北克拉通东部大地构造简图[31](a)与淮北煤田基岩构造纲要图[34](b)

    Figure 1.  Tectonic map of eastern North China Craton (a) and outline map of bedrock structures in the Huaibei Coalfield (b)

    图 2  钱营孜矿井三维地震-650 m水平切面图

    N.断层数量; H.落差(m)

    Figure 2.  Structural outline map interpreted from the -650 m horizontal seismic section of the Qianyingzi Coalmine

    图 3  钱营孜矿井地震勘探地质解译剖面图(剖面位置见图 2)

    Figure 3.  Geological cross-sections interpreted from the seismic profiles in the Qianyingzi Coalmine

    图 4  钱营孜矿井控煤构造样式剖面(a~f)及平面(g)示意图

    a~c.挤压构造组合样式; d~f.伸展构造组合样式; g.走滑构造组合样式

    Figure 4.  Seismic profiles (a-f) and ichnograph (g) of coal-controlled structural patterns in the Qianyingzi Coalmine

    图 5  钱营孜矿井主要褶皱与断层叠加变形过程示意图

    a.第1期NWW-SEE向挤压应力作用下发育了NNE轴向的冯家向斜,与淮北煤田宿南向斜、宿南背斜、南坪向斜等宽缓短轴褶皱同期;b.第2期近EW向挤压应力作用下发育了一系列近NS向逆断层,分割错断了冯家向斜,与整体向西逆冲缩短的徐宿弧形推覆构造同期;c.第3期NW-SE向挤压应力作用下,NNE向的F17断层南段出现左行压扭活动,同时共生、伴生大量的NE向的逆断层和NE轴向的东坪集背斜、李寨向斜等次级褶曲,NE向逆断层错断第2期近NS向逆断层;d.第4期近EW向的拉张应力作用下发育了近NS向正断层,正断层F22错断了第3期NE向逆断层(如F51);e.第5期NW-SE向拉张应力作用下发育了大量NE-SW向正断层,南坪断层和双堆断层分割错断了早期逆断层以及第4期F22断层,南坪断层的正断活动还控制了古近系沉积,但未切割新近系

    Figure 5.  Schematic diagrams of the development history of major folds and faults in the Qianyingzi Coalmine

    表  1  钱营孜矿井主要断层特征统计

    Table  1.   Statistics of major fault characteristics in the Qianyingzi Coalmine

    断层名称 断层性质 位置 构造分级 走向 倾向 倾角/(°) 最大落差/m 区内延伸长度/m
    南坪断层 正断层 西部边界 一级 NE NW 70 >1 000 75 000
    双堆断层 正断层 东南边界 一级 NE NW 70 >1 000 >3 000
    F22 正断层 冯家向斜西翼 二级 NS W 65~75 350 >6 500
    DF200 逆断层 东部边界 二级 NS E 45~50 >1 500 10 000
    QSF211 逆断层 邻近东部边界 三级 NS W 35~55 200 3 000
    F25 逆断层 邻近西部边界 三级 NE SE 45~50 160 5 000
    F51 逆断层 冯家向斜西翼 三级 NE SE 50~55 135 3 000
    F15 逆断层 冯家向斜西翼 三级 NS W 45~50 65 3 400
    F17 逆断层 冯家向斜东翼 二级 NS~NNE E~SEE 50~55 300 10 000
    F17-1 逆断层 F17断层东盘 三级 NNE SEE 50~55 110 3 900
    F17-2 逆断层 F17断层西盘 三级 NNE SEE 50~55 135 3 900
    DF165 逆断层 F17断层东盘 三级 NNE NWW 50~55 55 1 700
    QSF189 逆断层 F17断层东盘 三级 NE SE 35~55 80 1 700
    下载: 导出CSV

    表  2  钱营孜矿井控煤构造样式类型

    Table  2.   Classification of coal-controlled structural patterns in the Qianyingzi Coalmine

    类型 亚类型 控煤作用
    挤压构造组合样式 逆冲牵引褶皱 逆断层上、下盘的煤层均呈不对称褶皱变形,上盘煤层整体埋深变浅,靠近逆断层煤层揉皱变形强烈,层厚不稳定
    对冲式构造 对冲的逆断层上盘煤层因抬升变浅,所夹共用下降盘的煤层被掩覆,且多呈向形弯曲
    冲起构造 冲起断块内的煤层因进一步抬升而变浅,且多呈背形弯曲
    叠瓦状组合 含煤地层整体被抬升,但被分割成若干断块,断块内煤层产状改造显著,常伴生较多次级逆断层,构造较复杂
    伸展构造组合样式 地堑 地堑内煤层埋深增大,整体对煤层产状影响不大
    地垒 地垒上的煤层因抬升变浅,整体对煤层产状影响不大
    阶梯状断层 含煤地层被分割成若干断块,埋深依次加大,断块内煤层产状变化不大
    走滑构造组合样式 正花状构造 构造带内含煤地层整体呈背形弯曲,抬升变浅,伴生较多次级逆断层,构造复杂,靠近断层产状改造显著
    羽状雁列式构造 靠近主干断层的含煤地层破坏程度增大,构造复杂;平行于主干断层的剖面上,含煤地层可呈次级叠瓦状构造组合;垂直于主干断层的剖面上,含煤地层呈冲起构造组合或正花状构造组合特征
    下载: 导出CSV
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  • 收稿日期:  2023-07-25
  • 录用日期:  2023-10-07
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