平顶山矿区构造应力场演化规律及分布特征

Abstract
Figure/Table
References (0)
Related Citation (15)

Download: PDF (1892 KB) HTML (1 KB)
Export: BibTeX | EndNote (RIS)

Abstract To investigate the evolution pattern and distribution characteristics of tectonic stress field in Pingdingshan mining area，based on conjugate shear joints，fault slickenside and structure of the mining area data，the Stereographic projection method was applied to restore the direction of the paleotectonic stress in the research area. The characteristics and evolution pattern of the paleotectonic stress field were analyzed. By means of collecting in-situ stress and focal mechanism solution data，the tectonophysics and rock mechanics methods were applied to analyze the magnitude and direction of the present tectonic stress. The distribution characteristics and partitioned graph of the present tectonic stress field were got. The reconstruction results of the paleotectonic stress field showed that the mining area mainly got through three periods of tectonic stress field movement including Indosinian period，Yanshanian period(including Early and Late period) and Himalayan period. The directions of the maximum principal stress were nearly NS，NW，NE and NNE，respectively. The preferred attitudes of the directions were 3°∠6°，313°∠13°，54°∠9° and 18°∠15°. Under multistage tectonic stress field，Pingdingshan mining area formed geological structure on a series of NWW–NW directions folds and faults with NNE–NE directions secondary faults under the control of Likou syncline. The analytical results of the present tectonic stress field showed that the mine area has the partitioned characteristics. As the whole，the mining area manifests as dynamic stress field. The stress field type of the normal fault dominates absolutely in the west mining area. The stress field type of the strike-slip fault dominates absolutely in the middle mining area. The stress field type of the reverse fault and the strike-slip fault dominates in the east mining area. The mining area belongs to high stress region. In the regional mining area，the trend of the stress value is in a gradually increasing process from the west area to the east area. The stability of the stress field is between the relative stable state and the critical state. The maximum horizontal principal stress direction is NEE. The direction of the principle stress have undergone obvious changes in near faults. With the increasing of the buried deepness，the principal stress is gradually increasing，the coefficient of the horizontal pressure is decreasing，and the stress field has the changing tendency from dynamic to static. Research results provide the scientific basis for guiding mine roadway layout and preventing coal and rock dynamic disaster in mining area.

Key words： mining engineering Pingdingshan mining area tectonic stress field tectonic analysis evolution pattern distribution characteristics

	Service

	E-mail this article
	Add to my bookshelf
	Add to citation manager
	E-mail Alert
	RSS
	Articles by authors
	GUO Deyong1
	CHUAI Xiaosheng1
	ZHANG Jianguo2
	ZHANG Haoquan2

Cite this article:

GUO Deyong1,CHUAI Xiaosheng1,ZHANG Jianguo2, et al. The evolution pattern and distribution characteristics of tectonic stress#br# field in Pingdingshan mining area[J]. , 2022, 41(6): 1208-1222.

URL:

https://rockmech.whrsm.ac.cn/EN/Y2022/V41/I6/1208

[1] 袁亮. 深部采动响应与灾害防控研究进展[J]. 煤炭学报，2021，46(3)：716–725.(YUAN Liang. Research progress of mining response and disaster prevention and control in deep coal mines[J]. Journal of China Coal Society，2021，46(3)：716–725.(in Chinese))
[2] 郭德勇，韩德馨，王新义. 煤与瓦斯突出的构造物理环境及其应用[J]. 北京科技大学学报，2002，24(6)：581–584.(GUO Deyong，HAN Dexin，WANG Xinyi. Outburst-prone tectonophisical environment and its Applications[J]. Journal of University of Science and Technology Beijing，2002，24(6)：581–584.(in Chinese))
[3] 何满潮，谢和平，彭苏萍，等. 深部开采岩体力学研究[J]. 岩石力学与工程学报，2005，24(16)：2 803–2 813.(HE Manchao，XIE Heping，PENG Suping. Study on rock mechanics in deep mining engineering[J]. Chinese Journal of Rock Mechanics and Engineering，2005，24(16)：2 803–2 813.(in Chinese))
[4] 万天丰. 中国大地构造学[M]. 北京：地质出版社，2011：9–26.(WAN Tianfeng. The tectonics of China[M]. Beijing：Geological Publishing House，2011：9–26.(in Chinese))
[5] 曹代勇. 试论煤田构造应力场研究的形变标志物[J]. 煤炭学报，1991，16(1)：73–80.(CAO Daiyong. Deformation indicators for study of tectonic stresses field in coal fields[J]. Journal of China Coal Society，1991，16(1)：73–80.(in Chinese))
[6] CARVALHO J M F. Jointing patterns and tectonic evolution of the Maciço Calcário Estremenho，Lusitanian Basin，Portugal[J]. Journal of Structural Geology，2018，110(5)：155–171.
[7] SCHEIDEGGER A E. Surface joint systems，tectonic stresses and geomorphology：a reconciliation of conflicting observations[J]. Geomorphology，2001，38(3)：213–219.
[8] KAMIYA N，YAMAMOTO Y，WANG Q，et al. Major variations in vitrinite reflectance and consolidation characteristics within a post-middle Miocene forearc basin，central Japan：a geodynamical implication for basin evolution[J]. Tectonophysics，2017，710–711：69–80.
[9] FERRARI F，ZIEGLER M，APUANI T，et al. Geostatistical analyses of exfoliation and tectonic joint set spacing in alpine granites(Aar Valley，Switzerland)[J]. Bulletin of Engineering Geology and the Environment，2019，78(3)：1 645–1 668.
[10] 孙宗颀，张景和. 地应力在地质断层构造发生前后的变化[J]. 岩石力学与工程学报，2004，23(23)：3 964–3 969.(SUN Zongqi，ZHANG Jinghe. Variation of in-situ stresses before and after occurrence of geologic fault structure[J]. Chinese Journal of Rock Mechanics and Engineering，2004，23(23)：3 964–3 969.(in Chinese))
[11] GRIGGS D T，TURNER F J，HEARD H C. Deformation of rocks at 500 ℃ to 800 ℃[J]. Geological Society of America Memoirs，1960，79(9)：39–104.
[12] SCHOLZ C H. Shear heating and the state of stress on faults[J]. Journal of Geophysical Research Atmospheres，1980，85(B11)：6 174–6 184.
[13] 王茜茜，万天丰，袁玉松，等. 鄂西地区燕山期古构造应力场初步定量研究[J]. 地学前缘，2016，23(2)：269–279.(WANG Qianqian，WAN Tianfeng，YUAN Yusong，et al. The preliminary quantitative study of paleo teconic stress field of Yanshanian period in western Hubei Province[J]. Earth Science Frontiers，2016，23(2)：269–279.(in Chinese))
[14] 张泓，孟召平，何宗莲. 鄂尔多斯煤盆地构造应力场研究[J]. 煤炭学报，2000，25(增1)：1–5.(ZHANG Hong，MENG Zhaoping，HE Zonglian. Study on the tectonic stress fields in the Ordos Coal Basin[J]. Journal of China Coal Society，2000，25(Supp.1)：1–5.(in Chinese))
[15] 康红普，林健，张晓. 深部矿井地应力测量方法研究与应用[J]. 岩石力学与工程学报，2007，26(5)：929–933.(KANG Hongpu，LIN Jian，ZHANG Xiao. Research and application of in-situ stress measurement in deep mines[J]. Chinese Journal of Rock Mechanics and Engineering，2007，26(5)：929–933.(in Chinese))
[16] 蔡美峰，刘卫东，李远. 玲珑金矿深部地应力测量及矿区地应力场分布规律[J]. 岩石力学与工程学报，2010，29(2)：227–233.(CAI Meifeng，LIU Weidong，LI Yuan. In-situ stress measurement at deep position of Linglong gold mine and distribution law of in-situ stress field in mine area[J]. Chinese Journal of Rock Mechanics and Engineering，2010，29(2)：227–233.(in Chinese))
[17] LI P，CAI M F，GUO Q F，et al. In situ stress state of the northwest region of the Jiaodong Peninsula，China from overcoring stress measurements in Three Gold Mines[J]. Rock Mechanics and Rock Engineering，2019，52(11)：4 497–4 507.
[18] YIN S，XIE R C，WU Z H，et al. In situ stress heterogeneity in a highly developed strike-slip fault zone and its effect on the distribution of tight gases：A 3D finite element simulation study[J]. Marine and Petroleum Geology，2019，99(1)：75–91.
[19] ZHAO H J，MA F S，XU J M，et al. In situ stress field inversion and its application in mining-induced rock mass movement[J]. International Journal of Rock Mechanics and Mining Sciences，2012，53：120–128.
[20] GUO P，YAO L H，REN D S. Simulation of three-dimensional tectonic stress fields and quantitative prediction of tectonic fracture within the Damintun Depression，Liaohe Basin，northeast China[J]. Journal of Structural Geology，2016，86(5)：211–223.
[21] FENG J W，SHANG L，LI X Z，et al. 3D numerical simulation of heterogeneous in situ stress field in low-permeability reservoirs[J]. Petroleum Science，2019，16(5)：939–955.
[22] 张子敏，吴吟. 中国煤矿瓦斯赋存构造逐级控制规律与分区划分[J]. 地学前缘，2013，20(2)：237–245.(ZHANG Zimin，WU Yin. Tectonic-level-control rule and area-dividing of coalmine gas occurrence in China[J]. Earth Science Frontiers，2013，20(2)：237–245.(in Chinese))
[23] 张国伟，张本仁，袁学城. 秦岭造山带与大陆动力学[M]. 北京：科学出版社，2001：118–154.(ZHANG Guowei，ZHANG Benren，YUAN Xuecheng. Qinling Orogenic belt and continental dynamics[M]. Beijing：Science Press，2001：118–154.(in Chinese))
[24] EYAL Y，GROSS M R，ENGELDER T，et al. Joint development during fluctuation of the regional stress field in southern Israel[J]. Journal of Structural Geology，2001，23(2)：279–296.
[25] 河南煤田地质公司. 河南省晚古生代聚煤规律[M]. 武汉：中国地质大学出版社，1991：185–194.(Henan Mining Geology Inc.. Coal formation theory in Henan Province[M]. Wuhan：China University of Geosciences Press，1991：185–194.(in Chinese))
[26] 闫江伟. 地质构造对平顶山矿区煤与瓦斯突出的主控作用研究[博士学位论文][D]. 焦作：河南理工大学，2016.(YAN Jiangwei. Study on controlling effect of tectonic structures on coal and gas outburst in the Pingdingshan Mining Area[Ph. D. Thesis][D]. Jiaozuo：Henan Polytechnic University，2016.(in Chinese))
[27] 王迎超，靖洪文，陈坤福，等. 平顶山矿区地应力分布规律与空间区划研究[J]. 岩石力学与工程学报，2014，33(增1)：2 620–2 627. (WANG Yingchao，JING Hongwen，CHEN Kunfu，et al. Study of distribution regularities and regional division of in-situ stresses for Pingdingshan ming area[J]. Chinese Journal of Rock Mechanics and Engineering，2014，33(Supp.1)：2 620–2 627.(in Chinese))
[28] 沈荣喜，侯振海，王恩元，等. 基于三向应力监测装置的地应力测量方法研究[J]. 岩石力学与工程学报，2019，38(增2)：3 618–3 624. (SHEN Rongxi，HOU Zhenhai，WANG Enyuan，et al. Research on in-situ stress measurement method based on three-dimensional stress monitoring device[J]. Chinese Journal of Rock Mechanics and Engineering，2019，38(Supp.2)：3 618–3 624.(in Chinese))
[29] 王平. 地质力学方法研究——不同构造力作用下地应力的类型和分布[J]. 石油学报，1992，13(1)：1–12.(WANG Ping. A geomechanical technique-types and distribution of geostress under various tectonic forces[J]. Acta Petrolei Sinica，1992，13(1)：1–12.(in Chinese))
[30] 姚瑞，杨树新，陆远忠，等. 在地应力测量中准确求解最大、最小水平应力问题的探讨[J]. 岩土工程学报，2012，34(2)：317–325. (YAO Rui，YANG Shuxin，LU Yuanzhong，et al. Computing maximum and minimum horizontal stresses in in-situ stress measurement[J]. Chinese Journal of Geotechnical Engineering，2012，34(2)：317–325. (in Chinese))
[31] 莘海亮，方盛明，樊计昌，等. 豫北及邻区中小地震震源机制解及应力场反演[J]. 地震研究，2012，35(2)：184–189.(SHEN Hailiang，FANG Shengming，FAN Jichang，et al. Focal mechanism solution and stress field inversion of small and moderate earthquakes in North Henan and its adjacent region[J]. Journal of Seismological Research，2012，35(2)：184–189.(in Chinese))
[32] 林德超，裴放，李潇丽，等. 河南省区域地质概况[J]. 地质通报，1998，17(4)：337–346.(LIN Dechao，PEI Fang，LI Xiaoli，et al. Regional geological survey of Henan province[J]. Geological Bulletin of China，1998，17(4)：337–346.(in Chinese))
[33] 李鹏，郭奇峰，刘洪涛，等. 山东地区现今地应力场特征与应力积累水平分析[J]. 岩石力学与工程学报，2017，36(9)：2 220–2 231. (LI Peng，GUO Qifeng，LIU Hongtao，et al. Characteristics of current in-situ stress field and stress accumulation in Shandong region[J]. Chinese Journal of Rock Mechanics and Engineering，2017，36(9)：2 220–2 231.(in Chinese))
[34] 郭德勇，韩德馨. 地质构造控制煤和瓦斯突出作用类型研究[J]. 煤炭学报，1998，23(4)：337–341.(GUO Deyong，HAN Dexin. Research on the types of geological structure controlling coal-gas outbursts[J]. Journal of China Coal Society，1998，23(4)：337–341.(in Chinese))
[35] 谢富仁，崔效锋，赵建涛，等. 中国大陆及邻区现代构造应力场分区[J]. 地球物理学报，2004，47(4)：654–662.(XIE Furen，CUI Xiaofeng，ZHAO Jiantao，et al. Regional division of the recent tectonic stress field in China and adjacent[J]. Chinese Journal of Geophysics，2004，47(4)：654–662.(in Chinese))