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Cathodoluminescence of authigenic albite
Authors:Detlev K Richter  Thomas G  tte and Dirk Habermann
Institution:

a Institute of Geology, Mineralogy and Geophysics, Ruhr-University Bochum, Germany

b Institute of Experimental Physics, TU Freiberg, Germany

Abstract:Authigenic albites in carbonate rocks typically grow in a high-grade diagenetic to low-grade metamorphic environment and often show Roc-Tourné-twinning sensu Füchtbauer. Based on an investigation of four Middle to South European occurrences, they show Mn2+- and Fe3+-activated cathodoluminescence (CL), as revealed by combined high resolution spectroscopy of cathodoluminescence emission (HRS-CL), electron paramagnetic resonance (EPR), and proton-induced X-ray emission (μPIXE).
Keywords:Authigenic albite  Cathodoluminescence  Hot-cathode CL-microscopy  CL emission spectra  Mn2+ and Fe3+activation
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