Fabric transitions in quartz via viscoplastic self-consistent modeling part I: Axial compression and simple shear under constant strain

Quartz is a common crustal mineral that deforms plastically in a wide range of temperatures and pressures, leading to the development of different types of crystallographic preferred orientation (CPO) patterns. In this contribution we present the results of an extensive modeling of quartz fabric tra...

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Veröffentlicht in:Tectonophysics 2014-12, Vol.636, p.52-69
Hauptverfasser: Morales, Luiz F.G., Lloyd, Geoffrey E., Mainprice, David
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Sprache:eng
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