| 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, 
											