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Quartz is the most abundant single mineral in the earth's crust (although behind the feldspar group when taken collectively), and as such is present in a very large proportion of rocks both as primary crystals and as detrital grains in sedimentary and metamorphic rocks. Dynamic recrystallization is a process of crystal regrowth under conditions of stress and elevated temperature, commonly applied in the fields of metallurgy and materials science. Dynamic quartz recrystallization happens in a relatively predictable way with relation to temperature, and given its abundance quartz recrystallization can be used to easily determine relative temperature profiles, for example in orogenic belts or near intrusions.

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  • Dynamic quartz recrystallization (en)
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  • Quartz is the most abundant single mineral in the earth's crust (although behind the feldspar group when taken collectively), and as such is present in a very large proportion of rocks both as primary crystals and as detrital grains in sedimentary and metamorphic rocks. Dynamic recrystallization is a process of crystal regrowth under conditions of stress and elevated temperature, commonly applied in the fields of metallurgy and materials science. Dynamic quartz recrystallization happens in a relatively predictable way with relation to temperature, and given its abundance quartz recrystallization can be used to easily determine relative temperature profiles, for example in orogenic belts or near intrusions. (en)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/Bulging_Recrystallized_Quartzite.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Pabbar_GBM_Scale_Bar.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Pabbar_SGR.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Stages_of_Recrystallization.jpg
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  • Quartz is the most abundant single mineral in the earth's crust (although behind the feldspar group when taken collectively), and as such is present in a very large proportion of rocks both as primary crystals and as detrital grains in sedimentary and metamorphic rocks. Dynamic recrystallization is a process of crystal regrowth under conditions of stress and elevated temperature, commonly applied in the fields of metallurgy and materials science. Dynamic quartz recrystallization happens in a relatively predictable way with relation to temperature, and given its abundance quartz recrystallization can be used to easily determine relative temperature profiles, for example in orogenic belts or near intrusions. (en)
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