Mechanical genesis of Henan (China) Yima thrust nappe structure

被引:12
作者
Cai Wu [1 ]
Dou Lin-ming [1 ]
He Jiang [1 ]
Liu Hai-shun [2 ]
Li Zhen-lei [1 ]
Ding Yan-lu [1 ]
机构
[1] China Univ Min & Technol, State Key Lab Coal Resources & Safe Min, Xuzhou 221116, Peoples R China
[2] China Univ Min & Technol, Sch Sci, Xuzhou 221116, Peoples R China
基金
中国国家自然科学基金;
关键词
mechanical genesis; thrust nappe structure; centrifugal inertia force; fault mechanics; slip-line field theory; Coulomb's law of friction; LINE FIELD-THEORY; EARTH ROTATION; SLIP; TECTONICS;
D O I
10.1007/s11771-014-2251-6
中图分类号
TF [冶金工业];
学科分类号
080601 [冶金物理化学];
摘要
Considering the serious coal and rock dynamic disasters around the main slip plane called F16 in the coal mining area) of Henan Yima (China) thrust nappe structure, the mechanical genesis of the Yima thrust nappe structure was studied comprehensively using geomechanics, fault mechanics, elastic mechanics, and Coulomb's law of friction. First, using the centrifugal inertia force of Earth's rotation as a source, a mechanical model of N-S compression superimposed with W-E reverse torsion was established to explain the formation of the early Yima coal basin and Jurassic Yima Group coal measures. Second, an equation for the ultimate stress in the forming stage of F16 was derived using the plastic slip-line field theory and the parabolic Mohr failure criterion. Moreover, the distribution of ultimate stress and the geometric characteristics of the fault profile were obtained using the field model parameters. Finally, the stress field of F16 and the mechanical genesis of the large-scale reverse thrust sheet were discussed based on elastic mechanics theory and Coulomb's law of friction. The results show that the tectonic framework of the early Yima coal basin and the formation pattern of Jurassic Yima Group coal measures given by the model are consistent with the in-situ explorations. The geometric characteristics of the fault profile obtained by numerical calculation can better reflect the shape of F16 in its forming stage, and the mechanical genesis of the large-scale reverse thrust sheet also concurred with the field situations. Thus, this work can provide a foundation for further studies on the genesis of the thrust nappe structure, the mechanism of rock bursts induced by F16, and the characteristics of the residual stress field in the Yima mining area.
引用
收藏
页码:2857 / 2865
页数:9
相关论文
共 35 条
[1]
FRICTION OF ROCKS [J].
BYERLEE, J .
PURE AND APPLIED GEOPHYSICS, 1978, 116 (4-5) :615-626
[2]
Cai MF, 2002, ROCK MECH ENG, P219
[3]
CAO Dai-yong, 1988, COAL GEOLOGY EXPLORA, P11
[4]
CAO Dai-yong, 1992, J CHINA U MINING TEC, V3, P103
[5]
CHEN Chuan-shi, 1989, HENAN GEOLOGY, V7, P37
[6]
CHEN Chuan-shi, 1991, HENAN GEOLOGY, V9, P31
[7]
Chen Qiang, 1986, Seismology and Geology, V8, P11
[8]
The enhancement of seismicity before the 2004 Mw9.0 Indonesia Sumatra earthquake and its relation to the earth rotation [J].
Chen Xue-Zhong ;
Li Yan-E ;
Wang Heng-Xin ;
Guo Xiang-Yun .
CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION, 2013, 56 (01) :79-90
[9]
Crans W., 1980, J PETROL GEOL, V2, P265, DOI DOI 10.1111/J.1747-5457.1980.TB00707.X
[10]
Relationships between thrusts and normal faults in curved belts: New insight in the inversion tectonics of the Central-Northern Apennines (Italy) [J].
Di Domenica, Alessandra ;
Turtu, Antonio ;
Satolli, Sara ;
Calamita, Fernando .
JOURNAL OF STRUCTURAL GEOLOGY, 2012, 42 :104-117