Steady-State Preferred Orientation of Ice Deformed in Plane Strain at –1°C
نویسندگان
چکیده
منابع مشابه
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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The microstructures of eutectics between compounds were studied for systems MnO-MnS, NaCl-NaF, NaBr-NaF, LiF-NaF, and FeO-FeS. With the exception of FeS, all the compounds had the NaC1-type structure. In the systems having only NaC1-type structures, the lamellas of the two eutectic phases had matching crystal orientations. There was less consistency among the eutectic systems, however, than bet...
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ژورنال
عنوان ژورنال: Journal of Glaciology
سال: 1982
ISSN: 0022-1430,1727-5652
DOI: 10.3189/s0022143000011850