Article ID Journal Published Year Pages File Type
4733469 Journal of Structural Geology 2011 12 Pages PDF
Abstract
► Obtuse angles in the σ1-direction are characteristic of conjugate ductile shear zones. ► Most geologists regard them as result of progressive deformation. ► The MEM criterion, however, states that the angles (usually ∼110°) are original features. ► The 110° seems to be a material-invariant for the scale-range of 10−7-106 m.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geology
Authors
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