منابع مشابه
Acoustic Double Refraction in Low-porosity Rocks by Terry Todd, Gene Simmons, and W. Scott Baldridge
Anisotropy in physical properties of rocks can arise from preferred mineral orientation, mineral layering, nonhydrostatic stress, and anisotropic crack distribution. For instance, all of the following cause acoustic double refraction: preferential orientation of olivine grains in dunites, alternating layers in laboratory-sizedsamples of such mineral pairs as olivine-feldspar, wollastonite-diops...
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ژورنال
عنوان ژورنال: American Entomologist
سال: 1996
ISSN: 2155-9902,1046-2821
DOI: 10.1093/ae/42.1.64a