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- W2012126676 abstract "Petrofabrics, microstructures and dislocation substructures were investigated in the chlorite peridotite mylonite rim around the garnet peridotite of Alpe Arami (Ticino, Switzerland). The mylonite is a foliated rock containing strained relict porphyroclasts embedded in abundant recrystallized matrix material. The porphyroclasts exhibit a preferred orientation (the [1000]-fabric) of [100] perpendicular to the foliation and [010] together with [001] in the foliation, while the matrix developed a completely different pattern (the [010]-fabric) of [010] perpendicular to the foliation with [100] and [001] in this plane. The [100]-fabric, inherited from a neighbouring chlorite peridotite, is thought to represent a rotationally unstable orientation under deformation conditions present in the mylonite and was preserved from recrystallization because this orientation was unfavourable for deformation. The [010]-fabric represented a rotationally stable end orientation in respect to the strain axes, which could not be changed by further deformation. A sequence of microtextures of different stages in recrystallization of the porphyroclasts is discussed, representing fabric transitions from [100] to [010] perpendicular to the foliation depending on the strain conditions present in the matrix." @default.
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- W2012126676 date "1977-04-01" @default.
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- W2012126676 title "Fabric development of olivine in a peridotite mylonite" @default.
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- W2012126676 doi "https://doi.org/10.1016/0040-1951(77)90088-9" @default.
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