A new technique to automatically quantify microstructures of fine grained carbonate mylonites: two-step etching combined with SEM imaging and image analysis
暂无分享,去创建一个
[1] M. Handy,et al. The solid‐state flow of polymineralic rocks , 1990 .
[2] R. Heilbronner,et al. Fabric domains in quartz mylonites: localized three dimensional analysis of microstructure and texture , 1996 .
[3] J. Boland,et al. Superplastic flow in finegrained limestone , 1977 .
[4] J. M. Christie,et al. Chemical etching of deformation sub-structures in quartz , 1983 .
[5] O. Pfiffner. Deformation mechanisms and flow regimes in limestones from the Helvetic zone of the Swiss Alps , 1982 .
[6] E. Rutter. Use of extension testing to investigate the influence of finite strain on the Theological behaviour of marble , 1998 .
[7] J. Boland,et al. High temperature flow and dynamic recrystallization in carrara marble , 1980 .
[8] R. Heilbronner. Automatic grain boundary detection and grain size analysis using polarization micrographs or orientation images , 2000 .
[9] R. Panozzo. Two-dimensional analysis of shape-fabric using projections of digitized lines in a plane , 1983 .
[10] R. Panozzo. Two-dimensional strain from the orientation of lines in a plane , 1984 .
[11] B. Evans,et al. Grain growth in synthetic marbles with added mica and water , 1988 .
[12] C. Teyssier,et al. Thermomechanical evolution of a ductile duplex , 1997 .
[13] A. Ben. Marble mylonites in the Bancroft shear zone, Ontario, Canada: microstructures and deformation mechanisms , 1991 .
[14] K. Kunze,et al. Orientation imaging: The emergence of a new microscopy , 1993 .
[15] Patrick Trimby,et al. Microstructural imaging techniques: a comparison between light and scanning electron microscopy , 1999 .
[16] J. McArthur,et al. Experimental calcite fabrics in a synthetic weaker aggregate by coaxial and non-coaxial deformation , 1990 .
[17] D. Prior,et al. Orientation contrast imaging of microstructures in rocks using forescatter detectors in the scanning electron microscope , 1996, Mineralogical Magazine.
[18] R. Heilbronner,et al. The influence of three-dimensional grain size distributions on the rheology of polyphase rocks , 1998 .
[19] D. Olgaard. The role of second phase in localizing deformation , 1990, Geological Society, London, Special Publications.
[20] K. Kunze,et al. Texture of Solnhofen limestone deformed to high strains in torsion , 1998 .
[21] D. Dietrich,et al. Calcite fabrics in a natural shear environment, the Helvetic nappes of western Switzerland , 1984 .
[22] M. Handy,et al. The origin of shape preferred orientations in mylonite: inferences from in-situ experiments on polycrystalline norcamphor , 1998 .
[23] M. Burkhard. Calcite twins, their geometry, appearance and significance as stress-strain markers and indicators of tectonic regime : a review , 1993 .
[24] D. Bruhn,et al. Evidence for enhanced deformation in two-phase rocks: Experiments on the rheology of calcite-anhydrite aggregates , 1999 .
[25] S. Bauer,et al. Simple shear experiments on calcite rocks: rheology and microfabric , 1987 .
[26] E. Rutter,et al. Experimental study of grain-size sensitive flow of synthetic, hot-pressed calcite rocks , 1990, Geological Society, London, Special Publications.
[27] H. Exner,et al. Analysis of Grain- and Particle-Size Distributions in Metallic Materials , 1972 .
[28] Renée Heilbronner,et al. The autocorrelation function: an image processing tool for fabric analysis , 1992 .
[29] M. Burkhard. Ductile deformation mechanisms in micritic limestones naturally deformed at low temperatures (150–350°C) , 1990, Geological Society, London, Special Publications.