唐鑫, 朱炎铭, 赵少磊, 史乾. 开滦矿区唐山矿构造特征及成因演化[J]. 煤田地质与勘探, 2015, 43(1): 1-6. DOI: 10.3969/j.issn.1001-1986.2015.01.001
引用本文: 唐鑫, 朱炎铭, 赵少磊, 史乾. 开滦矿区唐山矿构造特征及成因演化[J]. 煤田地质与勘探, 2015, 43(1): 1-6. DOI: 10.3969/j.issn.1001-1986.2015.01.001
TANG Xin, ZHU Yanming, ZHAO Shaolei, SHI Qian. Tectonic characteristics and genetic evolution of Tangshan mine in Kailuan mining area[J]. COAL GEOLOGY & EXPLORATION, 2015, 43(1): 1-6. DOI: 10.3969/j.issn.1001-1986.2015.01.001
Citation: TANG Xin, ZHU Yanming, ZHAO Shaolei, SHI Qian. Tectonic characteristics and genetic evolution of Tangshan mine in Kailuan mining area[J]. COAL GEOLOGY & EXPLORATION, 2015, 43(1): 1-6. DOI: 10.3969/j.issn.1001-1986.2015.01.001

开滦矿区唐山矿构造特征及成因演化

Tectonic characteristics and genetic evolution of Tangshan mine in Kailuan mining area

  • 摘要: 开滦矿区唐山矿位于开平向斜北西翼,隶属燕山南麓赋煤构造带,由北向南依次发育FI、FII、FIII、FIV、FV主断层,地质构造复杂,控制了井田构造格局。基于钻孔和矿井地质资料,以构造规律解析为基础,结合平衡剖面技术,探讨了唐山矿现今构造特征及构造演化期次。研究结果显示:唐山矿主体构造形成于燕山期NW-SE向的挤压应力作用,动力来源为库拉-太平洋板块与欧亚大陆的相互挤压作用;喜马拉雅期,由于库拉-太平洋板块淹没于欧亚大陆之下,唐山矿受到NW-SE向的拉张应力作用,形成了一系列小型正断层,并导致FI逆断层发生构造反转而变为正断层;利用平衡剖面技术恢复了唐山矿构造演化过程,得到唐山矿地层缩短率为27.3%。

     

    Abstract: Located in the northern west wing of Kaiping syncline, Tangshan mine belongs to the south coal structural belt of Yanshan. In Tangshan mine field the main faults FI,FII,FIII,FIV and FV were developed from north to south, and the geological structure is complex. It also controls the mine tectonic framework. Based on the structure rule, combined with balanced section technique,the paper mainly discusses the current tectonic characteristics and tectonic evolution stage of Tangshan mine on the basis of the drilling and mine geological data. The research findings show:(1) The main structure of Tangshan mine has been affected by the NW-SE extrusion stress of Yanshanian, and the power source has been the compression of Kula Pacific plate and Eurasia. During Kula Himalayan period, because of the Pacific plate submerged beneath the Eurasia, in Tangshan mine effected by the NW-SE tensile stress, a series of small faults were formed and led to FI thrust tectonic inversion phenomenon turned into a normal fault. (2) This paper restores the tectonic evolution process of Tangshan mine by balanced section technique and acquires 27.3% shortening rate of Tangshan mine strata

     

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