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- W2015094885 abstract "Quartz textures measured from monomineralic veins within the Simplon Fault Zone show very similar patterns over a strike length of some 30 km. The c-axes form asymmetric, kinked single girdles, with variably developed vestiges of crossed girdle limbs. The kinking of the girdle may be controlled by the two c-axis orientations where double rhomb 〈a〉 slip is possible. A strong 〈a〉 maximum lies between 20° and 30° to the lineation in the XZ plane, which seems too large to be the angle to the bulk shear plane. Straight single girdle patterns may be possible for strict simple shear. In natural fault zones, where deformation is in general heterogeneous on all scales, kinked single girdles and Type I crossed girdle textures are much more common, perhaps because such textures provide more freedom to accommodate a general two-dimensional strain." @default.
- W2015094885 created "2016-06-24" @default.
- W2015094885 creator A5007726741 @default.
- W2015094885 date "1987-04-01" @default.
- W2015094885 modified "2023-10-02" @default.
- W2015094885 title "Quartz textures from the Simplon Fault Zone, southwest Switzerland and north Italy" @default.
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- W2015094885 doi "https://doi.org/10.1016/0040-1951(87)90157-0" @default.
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