Research paperDefect structure and deformation mechanisms in naturally deformed augite and enstatite
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Cited by (31)
Texture and elastic anisotropy of a mylonitic anorthosite from the Morin Shear Zone (Quebec, Canada)
2015, Journal of Structural GeologyCitation Excerpt :The crystallographic preferred orientation of clinopyroxene shows a distribution with (010) planes parallel to the foliation and [001] directions parallel to the rock lineation (Fig. 5B). This is a very common texture, both in natural and experimentally deformed clinopyroxene (e.g. Van Roermund and Boland, 1981; Van Roermund, 1983; Buatier et al., 1991; Skrotzki, 1994; Godard and Van Roermund, 1995; Bascou et al., 2001; Brenker et al., 2002). TEM investigations of omphacite (e.g. Godard and Van Roermund, 1995) and diopside (e.g. Amiguet et al., 2010) have not observed dislocation activity on the (010)[001] system.
Chapter 95 Dislocations in Minerals
2010, Dislocations in SolidsCitation Excerpt :Dislocations with [0 0 1] Burgers vectors dominate deformation with glide on the (1 0 0) and (0 1 0) planes [107–112]. There are also (1 0 0)[0 1 0] dislocations with a [1 0 0] line direction [311,312] [Fig. 13(a)]. The critical resolved shear stress (CRSS) for the (1 0 0)[0 0 1] slip system is significantly smaller than for (0 1 0)[0 0 1].
Deformation of diopside single crystal at mantle pressure. 1: Mechanical data
2009, Physics of the Earth and Planetary InteriorsProcesses controlling the shrinkage of porphyroclasts in gabbroic shear zones
2000, Journal of Structural GeologyDeformation-induced clinopyroxene fabrics from eclogites
1995, Journal of Structural GeologyEvolution of Microstructural Heterogeneity in the Deep Arc Lithosphere During Delamination
2023, Journal of Geophysical Research: Solid Earth
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Present address: Institut für Kristallographie und Festkörperphysik, Technische Universität Dresden, Mommsenstr. 13, 01062 Dresden, Germany.