Sliding-thrusting tectonics caused by thermal uplift in the Yunmeng Mountains, Beijing, China

Journal of Structural Geology

Volumn 10, Issue 2, 1988, Pages 135-144

  Zheng, Y ^a   Wang, Y ^a   Liu, R ^a   Shao, J ^a  

^a PEKING UNIVERSITY   (China)

Author keywords

[No Author keywords available]

Indexed keywords

GRANITE;

GEOLOGICAL FAULTS; SLIDING-THRUSTING TECTONICS; THERMAL UPLIFT; YUNMENG MOUNTAINS, CHINA;

GEOLOGY;

EID: 0023822696     PISSN: 01918141     EISSN: None     Source Type: Journal    
DOI: 10.1016/0191-8141(88)90111-3     Document Type: Article

References (17)

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7. A plane kinematic model of progressive deformation in a polycrystalline aggregate
8. The microstructure of the Shuiyu ductile normal fault zone in Huairou county of Beijing and the estimation of differential stresses
9. The simulation of fabric development during plastic deformation and its application to quartzite: the influence of deformation history
10. The reliability of asymmetric c-axis fabrics of quartz to determine sense of vorticity
11. The differentiation of oxygen isotope composition of the felsic mylonites in the Dashuiyu ductile shear zone (Huairou County, Beijing) and its geological significance
12. Microstructures of fault rocks in Beishicheng and Hefangkou fault zone, Beijing
13. An evaluation of criteria to deduce the sense of movement in sheared rocks
14. On features of mylonites in Hefangkou-Heishansi ductile fault zone, Huairou County, Beijing
15. On features of quartz fabric of mylonites in Shuiyu ductile fault, Huairou, Beijing
16. The ductile normal fault with low dip-angle and thrust in the Hefangkou area, Huairou County, Beijing