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- W2012308855 abstract "This paper reports the results of an attempt to identify the deformation micromechanisms in the brittle-ductile transition zone of the Alpine fault, New Zealand. Characterization of sequentially developed microstructures was carried out using optical microscopy, HVEM and STEM analysis. It was found that the transition zone corresponds to a broad zone of retrogression produced initially by microcracking and fluid infiltration. The non-catastropic nature of the fracturing indicates that fluid-enhanced sub-critical cracking is a significant crustal deformation mechanism. After the initial phase of retrogression, both ductile and brittle processes coexist and cyclically alternate in response to stress cycling. The relative importance of macroscopic brittle processes may decrease with time as more ductile minerals, especially phyllosilicates, develop during continued retrogression." @default.
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- W2012308855 date "1983-01-01" @default.
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- W2012308855 title "Semi-brittle deformation within the Alpine fault zone, New Zealand" @default.
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- W2012308855 doi "https://doi.org/10.1016/0191-8141(83)90070-6" @default.
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