Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4692672 | Tectonophysics | 2012 | 15 Pages |
Abstract
⺠Petrophysical anisotropies as reflecting petrofabric of weakly deformed sediments. ⺠Magnetic and electric anisotropy is controlled by the preferred orientation of phylosilicates. ⺠P-waves anisotropy is controlled by the orientation of porous space. ⺠The orientation of porous space is sensitive to the increase of layer parallel shortening (LPS). ⺠The void space is early controlled by deformation and is thus passively rotated during folding.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
P. Robion, F. Humbert, J.-C. Colombier, S. Leghay, D. Frizon de Lamotte,