Olivine-antigorite orientation relationships: Microstructures, phase boundary misorientations and the effect of cracks in the seismic properties of serpentinites
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[1] B. Reynard. Serpentine in active subduction zones , 2013 .
[2] H. Jung. Seismic anisotropy produced by serpentine in mantle wedge , 2011 .
[3] H. Wenk,et al. Elastic anisotropy modeling of Kimmeridge shale , 2013 .
[4] D. Mainprice,et al. Methods of calculating petrophysical properties from lattice preferred orientation data , 1994 .
[5] J. M. Brown,et al. The elastic constants of San Carlos olivine to 17 GPa , 1997 .
[6] H. Kern. P- and S-wave anisotropy and shear-wave splitting at pressure and temperature in possible mantle rocks and their relation to the rock fabric , 1993 .
[7] K. Michibayashi,et al. Trench-parallel anisotropy produced by serpentine deformation in the hydrated mantle wedge , 2009, Nature.
[8] G. B. Piccardo,et al. From magmatism through metamorphism to sea floor emplacement of subcontinental Adria lithosphere during pre-Alpine rifting (Malenco, Italy) , 1993 .
[9] A. Vauchez,et al. Feedback between melt percolation and deformation in an exhumed lithosphere asthenosphere boundary , 2008 .
[10] Jay D. Bass,et al. Elasticity of antigorite, seismic detection of serpentinites, and anisotropy in subduction zones , 2009 .
[11] J. Willis. Bounds and self-consistent estimates for the overall properties of anisotropic composites , 1977 .
[12] P. Ulmer,et al. Serpentine Stability to Mantle Depths and Subduction-Related Magmatism , 1995, Science.
[13] J. Crocker,et al. References and Notes Supporting Online Material Materials and Methods References Movies S1 and S2 the Subduction Zone Flow Field from Seismic Anisotropy: a Global View , 2022 .
[14] Simon M. Peacock,et al. Subduction factory 1. Theoretical mineralogy, densities, seismic wave speeds, and H 2 O contents , 2003 .
[15] M. Mookherjee,et al. Trench parallel anisotropy and large delay times: Elasticity and anisotropy of antigorite at high pressures , 2011 .
[16] R. Hill. The Elastic Behaviour of a Crystalline Aggregate , 1952 .
[17] M. Humbert,et al. On the Principle of a Geometric Mean of Even-Rank Symmetric Tensors for Textured Polycrystals , 1995 .
[18] P. V. Keken,et al. The structure and dynamics of the mantle wedge , 2003 .
[19] K. Michibayashi,et al. Reply to comment by Nozaka (2014) on “Dehydration breakdown of antigorite and the formation of B-type olivine CPO” , 2014 .
[20] David Mainprice,et al. Seismic properties and anisotropy of the continental crust: Predictions based on mineral texture and rock microstructure , 2017 .
[21] M. Long. CONSTRAINTS ON SUBDUCTION GEODYNAMICS FROM SEISMIC ANISOTROPY , 2013 .
[22] Hans-Rudolf Wenk,et al. Seismic anisotropy of serpentinite from Val Malenco, Italy , 2015 .
[23] B. W. Evans. The Serpentinite Multisystem Revisited: Chrysotile Is Metastable , 2004 .
[24] Zita Bukovská,et al. Pressure solution in rocks: focused ion beam/transmission electron microscopy study on orthogneiss from South Armorican Shear Zone, France , 2015, Contributions to Mineralogy and Petrology.
[25] J. Wookey,et al. Seismic evidence for flow in the hydrated mantle wedge of the Ryukyu subduction zone , 2016, Scientific Reports.
[26] V. Trommsdorff,et al. Antigorite polysomatism: behaviour during progressive metamorphism , 1987 .
[27] A. Morawiec. Distributions of Misorientation Angles and Misorientation Axes for Crystallites with Different Symmetries , 1997 .
[28] David Mainprice,et al. A FORTRAN program to calculate seismic anisotropy from the lattice preferred orientation of minerals , 1990 .
[29] Bin Liu,et al. Relationship between anisotropy of P and S wave velocities and anisotropy of attenuation in serpentinite and amphibolite , 1997 .
[30] G. Hirth,et al. Deformation of antigorite serpentinite at high temperature and pressure , 2010 .
[31] Simon M. Peacock,et al. Subduction factory 2. Are intermediate‐depth earthquakes in subducting slabs linked to metamorphic dehydration reactions? , 2003 .
[32] Richard Von Mises,et al. Mechanik der plastischen Formänderung von Kristallen , 1928 .
[33] B. Stöckhert,et al. Dissolution precipitation creep versus crystalline plasticity in high-pressure metamorphic serpentinites , 2011 .
[34] Simon M. Peacock,et al. Serpentinization of the forearc mantle , 2003 .
[35] T. Gerya,et al. Deep slab hydration induced by bending-related variations in tectonic pressure , 2009 .
[36] T. Mizukami,et al. Obliteration of olivine crystallographic preferred orientation patterns in subduction-related antigorite-bearing mantle peridotite: an example from the Higashi–Akaishi body, SW Japan , 2011 .
[37] M. Humbert,et al. The Realization of the Concept of a Geometric Mean for Calculating Physical Constants of Polycrystalline Materials , 1993 .
[38] F. Wicks,et al. Serpentine textures and serpentinization , 1977 .
[39] D. Mainprice,et al. Mica, deformation fabrics and the seismic properties of the continental crust , 2009 .
[40] J. Bass,et al. High‐pressure elasticity of serpentine and seismic properties of the hydrated mantle wedge , 2013 .
[41] G. Seward,et al. Seismic signatures of a hydrated mantle wedge from antigorite crystal-preferred orientation (CPO) , 2013 .
[42] B. Reynard,et al. Deformation mechanisms and rheology of serpentines in experiments and in nature , 2014 .
[43] G. Hirth,et al. Rheology and Tectonic Significance of Serpentinite , 2013 .
[44] B. Reynard,et al. Pressure-temperature estimates of the lizardite/antigorite transition in high pressure serpentinites , 2013 .
[45] C. Vollmer,et al. The legacy of crystal-plastic deformation in olivine: high-diffusivity pathways during serpentinization , 2012, Contributions to Mineralogy and Petrology.
[46] S. Speziale,et al. Structural insights and elasticity of single-crystal antigorite from high-pressure Raman and Brillouin spectroscopy measured in the (010) plane , 2015 .
[47] F. Brenker,et al. The application of electron backscatter diffraction and orientation contrast imaging in the SEM to textural problems in rocks , 1999 .
[48] H. Takagi,et al. Sequential deformation from serpentinite mylonite to metasomatic rocks along the Sashu Fault, SW Japan , 2010 .
[49] H. Iwamori. Transportation of H2O beneath the Japan arcs and its implications for global water circulation , 2007 .
[50] Helmut Schaeben,et al. Calculating anisotropic physical properties from texture data using the MTEX open-source package , 2011 .
[51] Don L. Anderson,et al. The effect of oriented cracks on seismic velocities , 1974 .
[52] D. Mainprice. Modelling the anisotropic seismic properties of partially molten rocks found at mid-ocean ridges , 1997 .
[53] K. Michibayashi,et al. A new method for calculating seismic velocities in rocks containing strongly dimensionally anisotropic mineral grains and its application to antigorite-bearing serpentinite mylonites , 2014 .
[54] B. Evans,et al. Effects of serpentinization on the lithospheric strength and the style of normal faulting at slow-spreading ridges , 1997 .
[55] Y. Chastel,et al. Viscoplastic self‐consistent and equilibrium‐based modeling of olivine lattice preferred orientations: Implications for the upper mantle seismic anisotropy , 2000 .
[56] Simon M. Peacock,et al. Hydrous minerals in the mantle wedge and the maximum depth of subduction thrust earthquakes , 1999 .
[57] G. Capitani,et al. The crystal structure of a second antigorite polysome (m = 16), by single-crystal synchrotron diffraction , 2006 .
[58] B. Reynard,et al. Electron back‐scattering diffraction (EBSD) measurements of antigorite lattice‐preferred orientations (LPO) , 2010, Journal of microscopy.
[59] R. Tibshirani,et al. An introduction to the bootstrap , 1993 .
[60] B. Reynard,et al. Tectonic significance of serpentinites , 2015 .
[61] A. Tommasi,et al. Plastic deformation and development of antigorite crystal preferred orientation in high-pressure serpentinites , 2012 .
[62] D. Marcotte,et al. Antigorite-induced seismic anisotropy and implications for deformation in subduction zones and the Tibetan Plateau , 2014 .
[63] R. Mclaughlin. A study of the differential scheme for composite materials , 1977 .
[64] N. Christensen,et al. Serpentinites, Peridotites, and Seismology , 2004 .
[65] Helmut Schaeben,et al. A novel pole figure inversion method: specification of the MTEX algorithm , 2008 .
[66] D. Mainprice. Seismic Anisotropy of the Deep Earth from a Mineral and Rock Physics Perspective , 2007 .
[67] D. Marcotte,et al. Seismic velocities, anisotropy, and shear‐wave splitting of antigorite serpentinites and tectonic implications for subduction zones , 2013 .
[68] Adam Morawiec,et al. Orientations and Rotations: Computations in Crystallographic Textures , 1999 .
[69] K. Michibayashi,et al. Spatial variations in antigorite fabric across a serpentinite subduction channel : Insights from the Ohmachi Seamount, Izu-Bonin frontal arc , 2010 .
[70] David Mainprice,et al. The influence of hydrous phases on the microstructure and seismic properties of a hydrated mantle rock , 2013 .
[71] J. B. Walsh. The effect of cracks on the compressibility of rock , 1965 .
[72] D. Mainprice,et al. Serpentine Mineral Replacements of Natural Olivine and their Seismic Implications: Oceanic Lizardite versus Subduction-Related Antigorite , 2010 .
[73] V. Vavryčuk,et al. Effect of pressure on 3D distribution of P-wave velocity and attenuation in antigorite serpentinite , 2017 .
[74] K. Kunze,et al. Orientation imaging: The emergence of a new microscopy , 1993 .
[75] B. Reynard,et al. High-Pressure Creep of Serpentine, Interseismic Deformation, and Initiation of Subduction , 2007, Science.
[76] P. Philippot,et al. Deep fluids in subduction zones , 2001 .
[77] H. Wenk,et al. Antigorite crystallographic preferred orientations in serpentinites from Japan , 2014 .
[78] Sean D. Barrett,et al. Image Analysis in Earth Sciences: Microstructures and Textures of Earth Materials , 2013 .
[79] H. Green. Shearing instabilities accompanying high-pressure phase transformations and the mechanics of deep earthquakes , 2007, Proceedings of the National Academy of Sciences.
[80] N. Christensen,et al. Compressional wave velocities in possible mantle rocks to pressures of 30 kilobars , 1974 .
[81] J. Escartín,et al. Deformation mechanisms of antigorite serpentinite at subduction zone conditions determined from experimentally and naturally deformed rocks , 2014 .
[82] B. Reynard,et al. Stability and dynamics of serpentinite layer in subduction zone , 2009 .
[83] B. W. Evans,et al. Titanian hydroxyl-clinohumite: Formation and breakdown in antigorite rocks (Malenco, Italy) , 1980 .