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Crystal preferred orientation of an amphibole experimentally deformed by simple shear
Seismic anisotropy has been widely observed in crust and mantle materials and plays a key role in the understanding of structure and flow patterns. Although seismic anisotropy can be explained by the crystal preferred orientation (CPO) of highly anisotropic minerals in the crust, that is, amphibole,...
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Pub. Group
2015
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4403317/ https://www.ncbi.nlm.nih.gov/pubmed/25858349 http://dx.doi.org/10.1038/ncomms7586 |