Seismic anisotropy from cores of hydrated, deep crustal mafic shear zones: implications for the relationship between strain, deformation mechanisms, and anisotropy magnitude

Cailey Brown Condit, University of Washington, Earth and Space Sciences, Seattle, United States, Kevin H Mahan, University of Colorado at Boulder, Geological Sciences, Boulder, United States, Vera Schulte-Pelkum, Univ Colorado Boulder, Boulder, United States and Omero Orlandini, University of Texas at Austin, Department of Geological Sciences, Austin, TX, United States
Back to: Seismic Anisotropy and Deformation in the Continental Crust II