$Polymineralic orientation analysis of magmatic rocks using Electron Back-Scatter Diffraction: Implications for igneous fabric origin and evolution$

Polymineralic orientation analysis of magmatic rocks using Electron Back-Scatter Diffraction: Implications for igneous fabric origin and evolution

Electron Back-Scatter Diffraction (EBSD), which provides an easy way of acquiring large numbers of individual crystallographic orientation data from different phases, has been applied to the study of magmatic fabrics. Using this technique, the crystallographic preferred orientation (CPO) of plagiocl...

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Veröffentlicht in:	Tectonophysics 2007-11, Vol.444 (1), p.45-62
Hauptverfasser:	Romeo, I., Capote, R., Lunar, R., Cayzer, N.
Format:	Artikel
Sprache:	eng
Schlagworte:	Crystallographic preferred orientation (CPO) Magmatic fabrics Shape preferred orientation (SPO) Structural geology
Online-Zugang:	Volltext
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