Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4733469 | Journal of Structural Geology | 2011 | 12 Pages |
Abstract
⺠Obtuse angles in the Ï1-direction are characteristic of conjugate ductile shear zones. ⺠Most geologists regard them as result of progressive deformation. ⺠The MEM criterion, however, states that the angles (usually â¼110°) are original features. ⺠The 110° seems to be a material-invariant for the scale-range of 10â7-106 m.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Yadong Zheng, Jinjiang Zhang, Tao Wang,