Titlebook: Atlas of Mylonites - and related microstructures; Rudolph A. J. Trouw,Cees W. Passchier,Dirk J. Wier Book 2010 Springer-Verlag Berlin Heid

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Introduction,ks (e.g. Shelley 1993; Snoke et al. 1998; Blenkinsop 2000; Vernon 2004; Passchier & Trouw 2005) and in many articles referred to in these books. Especially the excellent photographic atlas by Snoke et al. (1998) gives an extensive overview of current ideas on nomenclature and processes related to fa

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Low-Grade Mylonites,grade mylonites. Whereas many feldspar porphyroclasts in low-grade mylonites still show fracturing by cataclasis, the quartz is usually deformed by crystal-plastic processes as shown by its change in shape and by undulose extinction. At increasing temperature bulging recrystallisation starts to mani

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Protomylonite, Mylonite and Ultramylonite,bserved in low-grade mylonites where the percentage of porphyroclasts decreases progressively with strain intensity. However, the percentage of matrix is highly dependent on mineralogical composition (e.g. quartz and biotite tend to convert to matrix readily). Compositional banding in gneiss can the

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,“False” mylonites,is section. Low grade metasedimentary wackes containing detrital quartz grains in a fine-grained matrix may resemble mylonites. The quartz may show undulose extinction and resemble porphyroclasts in a mylonite (compare Fig. 10.2). However, in real mylonites quartz is the weaker mineral and tends to

Culmination

from what type of rock did this mylonite derive? What were the metamorphic circumstances during mylonitization? What was the intensity of deformation?, and What was the sense of shear?..This book will complement the very successful textbook "Microtectonics" by Passchier and Trouw..978-3-662-50192-4978-3-642-03608-8