Preferred orientation in experimentally deformed stishovite: implications for deformation mechanisms

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Preferred orientation in experimentally deformed stishovite: implications for deformation mechanisms

Stishovite is a polymorph of SiO2 present in the mantle, making its deformation properties relevant to Earth science. Stishovite was first produced experimentally (Stishov and Popova 1961) and found to have a rutile structure (space group P42/mnm, Stishov and Belov 1962; Sinclair and Ringwood 1978; Ross et al. 1990) with its silicon in octahedral rather than tetrahedral coordination, as is char...

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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, experimental studies on the CPO of amphibole are limited. Here we present the results of novel e...

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ژورنال

عنوان ژورنال: Physics and Chemistry of Minerals

سال: 2014

ISSN: 0342-1791,1432-2021

DOI: 10.1007/s00269-014-0718-5