Abstract

The study of deformation features has been of great importance to determine deformation mechanisms in quartz. Relevant microstructures in both growth and deformation processes include dislocations, subgrains, subgrain boundaries, Brazil and Dauphiné twins and planar deformation features (PDFs). Dislocations and twin boundaries are most commonly imaged using a transmission electron microscope (TEM), because these cannot directly be observed using light microscopy, in contrast to PDFs. Here, we show that red-filtered cathodoluminescence imaging in a scanning electron microscope (SEM) is a useful method to visualise subgrain boundaries, Brazil and Dauphiné twin boundaries. Because standard petrographic thin sections can be studied in the SEM, the observed structures can be directly and easily correlated to light microscopy studies. In contrast to TEM preparation methods, SEM techniques are non-destructive to the area of interest on a petrographic thin section.

Highlights

  • Quartz is one of the main constituents of crustal rocks, and its properties are very relevant to crustal deformation

  • We examine a range of quartz samples using composite colour scanning electron microscope (SEM)-CL, electron backscattered diffraction (EBSD), forescatter electron (FSE) and transmission electron microscope (TEM)

  • Correlation of images from SEM-CL with FSE, EBSD and TEM shows that red cathodoluminescence is associated with subgrain boundaries, twin boundaries and healed planar deformation features (PDFs) in quartz

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Summary

Introduction

Quartz is one of the main constituents of crustal rocks, and its properties are very relevant to crustal deformation. Microstructures in tectonically deformed quartz include dislocations, subgrains and various types of twins. Dislocations and subgrains can be used as palaeostress indicators (Twiss 1977; White 1979; Schmid et al 1980) Twinning occurs during both growth and deformation processes and includes Brazil and Dauphiné types. Dauphiné twins have received some interest in relation to shock effects in quartz (Chen et al 2011; Trepmann and Spray 2005; Wenk et al 2005, 2011), and basal Brazil twins are considered as diagnostic shock evidence (Goltrant et al 1991, 1992; Leroux and Doukhan 1996; Leroux et al 1994; Trepmann 2008; Trepmann and Spray 2006)

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