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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The Strong Degree and the FI-Degreeion of mylonites because of the contrasting behaviour of quartz and biotite on the one hand (forming matrix) and feldspar and muscovite on the other hand (forming porphyroclasts). Another group of rocks that readily forms mylonites are impure quartzites in which resistant minerals tend to form fish-

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The Strong Degree and the FI-DegreeThe temperature range for the formation of this group of mylonites is approximately 500 to 650 °C. In medium-grade mylonites quartz is usually fully recrystallised, mainly by subgrain rotation, and has grown to a polygonal crystalloblastic fabric of strain free grains with an average grain size exceeding about 50 micrometers.

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Functional Identities in (Semi)prime RingsThe purpose of this chapter is to give the reader the option to check his or her level of understanding of mylonites by trying to answer the questions given in the figure captions. Although we do not claim that our solutions given at the end of the chapter are the only possible ones, they will enable an assessment of the level of comprehension.

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