Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
809630 | International Journal of Rock Mechanics and Mining Sciences | 2013 | 8 Pages |
Abstract
Research highlights► The increased tensile stresses and the decreased and shear strength of the fault plane caused the occurrence of the fault reactivation. ► The shear displacements on the fault plane decrease with the depth of the fault, ending off downward to the end of the reactivated section. ► Under the assumption of linear elasticity, the ratio of the scarp lengths in any two stages is equal to the squared ratio of the reactivated lengths. ► The preliminary research are verified and discussed based on physical experiments.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geotechnical Engineering and Engineering Geology
Authors
Haijun Zhao, Fengshan Ma, Jiamo Xu, Jie Guo,