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- W2016129518 abstract "Strain measurements from quartz grain shapes in deformed Jura Quartzite around Loch Skerrols, Islay, SW Scotland, indicate that a strain gradient is associated with the Loch Skerrols Thrust which separates the Jura Quartzite from the Bowmore Sandstone. Progressive strain is associated with microstructural changes in the form of grain refinement through to dynamic recrystallization. The maximum observed ratio of intracrystalline strain is 1.9:1.3:0.4,ξσ = 1.1. The X-axis of the finite-strain ellipsoid is close to the mesoscopic lineation in quartz-mylonites in the thrust belt and the XY plane is sub-parallel to the foliation. The apparent flattening strain may be explained by superposition of simple shear (thrust regime) on initial flattening strain associated with the earlier stages of progressive development of the Islay Anticline. This implies that the Loch Skerrols Thrust is comparable to a break thrust. Strain-induced quartz c-axis preferred orientation increases in intensity as the thrust is approached. At a higher strain the fabric is a type-I cross-girdle pattern with a point maximum within 20° of Z. Fabric asymmetry, both internal and with respect to an external frame, defined by the principal strain directions, attests to a westward transport of Dalradian Jura Quartzite on the thrust." @default.
- W2016129518 created "2016-06-24" @default.
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- W2016129518 date "1989-01-01" @default.
- W2016129518 modified "2023-09-27" @default.
- W2016129518 title "The caledonian skerrols thrust, SW Scotland—microstructure and strain" @default.
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- W2016129518 doi "https://doi.org/10.1016/0191-8141(89)90087-4" @default.
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