Elasticity of glaucophane, seismic velocities and anisotropy of the subducted oceanic crust

[1]  R. Powell,et al.  Calculated phase equilibria for a morb composition in a P–T range, 450–650 °C and 18–28 kbar: the stability of eclogite , 2010 .

[2]  J. Nakajima,et al.  Tomographic imaging of hydrated crust and mantle in the subducting Pacific slab beneath Hokkaido, Japan: Evidence for dehydration embrittlement as a cause of intraslab earthquakes , 2009 .

[3]  Jay D. Bass,et al.  Elasticity of antigorite, seismic detection of serpentinites, and anisotropy in subduction zones , 2009 .

[4]  K. Michibayashi,et al.  Trench-parallel anisotropy produced by serpentine deformation in the hydrated mantle wedge , 2009, Nature.

[5]  J. Nakajima,et al.  Seismic evidence for thermally‐controlled dehydration reaction in subducting oceanic crust , 2009 .

[6]  D. Mainprice,et al.  B-type olivine fabrics developed in the fore-arc side of the mantle wedge along a subducting slab , 2008 .

[7]  D. Jenkins,et al.  Compressibility of synthetic glaucophane , 2008 .

[8]  H. Kawakatsu,et al.  Seismic Evidence for Deep-Water Transportation in the Mantle , 2007, Science.

[9]  D. Jenkins,et al.  Molar volume and thermal expansion of glaucophane , 2006 .

[10]  A. Liebscher,et al.  Physical and chemical properties of the epidote minerals: An introduction , 2004 .

[11]  D. Mainprice,et al.  Anisotropic seismic properties of the upper mantle beneath the Torre Alfina area (Northern Apennines, Central Italy) , 2003 .

[12]  J. Bascou,et al.  EBSD-measured lattice-preferred orientations and seismic properties of eclogites , 2001 .

[13]  J. Connolly,et al.  Metamorphic devolatilization of subducted oceanic metabasalts: implications for seismicity, arc magmatism and volatile recycling , 2001 .

[14]  S. Sinogeikin,et al.  Single-crystal elasticity of pyrope and MgO to 20 GPa by Brillouin scattering in the diamond cell , 2000 .

[15]  Y. Chastel,et al.  Viscoplastic self‐consistent and equilibrium‐based modeling of olivine lattice preferred orientations: Implications for the upper mantle seismic anisotropy , 2000 .

[16]  G. Abers.  Hydrated subducted crust at 100–250 km depth , 2000 .

[17]  W. Ernst,et al.  Overview of UHP Metamorphism and Tectonics in Well-Studied Collisional Orogens , 1999 .

[18]  H. Kern,et al.  Petrophysical studies on rocks from the Dabie ultrahigh-pressure (UHP) metamorphic belt , 1999 .

[19]  S. Poli,et al.  Experimentally based water budgets for dehydrating slabs and consequences for arc magma generation , 1998 .

[20]  W. Ernst,et al.  Buoyancy-driven, rapid exhumation of ultrahigh-pressure metamorphosed continental crust. , 1997, Proceedings of the National Academy of Sciences of the United States of America.

[21]  Ricardo A. Lebensohn,et al.  A self-consistent anisotropic approach for the simulation of plastic deformation and texture development of polycrystals : application to zirconium alloys , 1993 .

[22]  H. Kern,et al.  Pressure and temperature dependence of P- and S-wave velocities, seismic anisotropy and density of sheared rocks from the Sierra Alpujata massif (Ronda peridotites, Southern Spain) , 1993 .

[23]  J. Bass,et al.  Single‐crystal elastic properties of omphacite‐C2/c by Brillouin spectroscopy , 1992 .

[24]  M. Mellini,et al.  Compressibility and high pressure structure refinement of tremolite, pargasite and glaucophane , 1991 .

[25]  David Mainprice,et al.  A FORTRAN program to calculate seismic anisotropy from the lattice preferred orientation of minerals , 1990 .

[26]  J. Bass,et al.  Elasticity of a grossular-pyrope-almandine garnet , 1989 .

[27]  B. Reynard,et al.  Deformation Mechanisms In Naturally Deformed Glaucophanes - A Tem And Hrem Study , 1989 .

[28]  J. Bass.  Elasticity of grossular and spessartite garnets by Brillouin spectroscopy , 1989 .

[29]  Bernard J. Wood,et al.  Subduction zone thermal structure and mineralogy and their relationship to seismic wave reflections and conversions at the slab/mantle interface , 1989 .

[30]  T. Duffy,et al.  Elasticity of enstatite and its relationship to crystal structure , 1986 .

[31]  Herbert R. Carleton,et al.  Elasticity of coesite , 1977 .

[32]  A. Nicolas,et al.  Deformation-Induced Recrystallization Due to Progressive Misorientation of Subgrains, with Special Reference to Mantle Peridotites , 1975, The Journal of Geology.

[33]  W. Ernst.  Blueschist metamorphism and P-T regimes in active subduction zones , 1973 .

[34]  R. N. Thurston,et al.  Elastic Moduli of Quartz versus Hydrostatic Pressure at 25 and-195.8C , 1965 .

[35]  N. C. Krieger Lassen,et al.  The relative precision of crystal orientations measured from electron backscattering patterns , 1996 .

[36]  J. R. Sandercock,et al.  Trends in brillouin scattering: Studies of opaque materials, supported films, and central modes , 1982 .

[37]  J. Kienast,et al.  Relations entre le metamorphisme et la deformation dans la zone Sesia-Lanzo (Alpes Occidentales) et le probleme de l'eclogitisation de la croute continentale , 1982 .

[38]  M. Musgrave,et al.  Crystal Acoustics: Introduction to the Study of Elastic Waves and Vibrations in Crystals , 1970 .