Research paperFrom qualitative to quantitative magnetic anisotropy analysis: The prospect of finite strain calibration
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Current challenges and future developments in magnetic fabric research
2020, TectonophysicsEvidence for non-coaxiality of ferrimagnetic and paramagnetic fabrics, developed during magma flow and cooling in a thick mafic dyke
2014, TectonophysicsCitation Excerpt :The superposition of magnetic fabrics, related to magnetic carriers with normal and inverse fabric, or with distinct preferred orientations and/or shapes, is one factor that can result in a whole-rock AMS fabric that does not reflect the true preferred orientation of minerals (Borradaile and Henry, 1997; Chadima et al., 2009; Fanjat et al., 2012; Ferré, 2002; Hirt and Almqvist, 2012; Lamali et al., 2013; Potter and Stephenson, 1988; Rochette, 1988; Rochette et al., 1999; Silva et al., 2008; Tarling and Hrouda, 1993). To decompose composite magnetic fabrics complementary experimental methods (e.g., anisotropy of magnetic remanence and high-field torque magnetometry) and analytical and computational solutions have been developed to separate sub-fabrics (e.g., Banerjee and Stacey, 1967; Callot and Guichet, 2003; Ferré et al., 2004; Jelinek, 1996; Kratinová et al., 2006, 2010; Henry, 1983, 1997; Henry and Daly, 1983; Hrouda and Jelinek, 1990; Martín-Hernandez and Garcia-Hernandez, 2010; Martín-Hernandez and Hirt, 2001, 2004; McCabe et al., 1985; Moreira et al., 1999; Roperch and Taylor, 1986; Schmidt et al., 2007; Stephenson, 1980; Stephenson et al., 1986). More recently, rock magnetic fabrics studies start to be complemented by quantitative microstructural and crystallographic preferred orientation analyses in order to better understand the rheological behaviour of rocks (e.g., Bascou et al., 2005; Boiron et al., 2013; Cifelli et al., 2009; Machek et al., 2014--this volume; Závada et al., 2007).