Water, partial melting and the origin of the seismic low velocity and high attenuation zone in the upper mantle

[1]  P. Dawson,et al.  Teleseismic imaging of subaxial flow at mid-ocean ridges: traveltime effects of anisotropic mineral texture in the mantle , 1996 .

[2]  T. Jordan,et al.  Seismic structure of the upper mantle in a central Pacific corridor , 1996 .

[3]  Greg Hirth,et al.  Water in the oceanic upper mantle: implications for rheology , 1996 .

[4]  B. Evans,et al.  Strength of the lithosphere: Constraints imposed by laboratory experiments , 1995 .

[5]  S. Karato,et al.  Lattice preferred orientation of olivine aggregates deformed in simple shear , 1995, Nature.

[6]  Greg Hirth,et al.  Experimental constraints on the dynamics of the partially molten upper mantle: Deformation in the diffusion creep regime , 1995 .

[7]  D. Forsyth,et al.  Geochemical constraints on initial and final depths of melting beneath mid-ocean ridges , 1995 .

[8]  A. Cazenave,et al.  Geoid lineations of 1000 km wavelength over the central Pacific , 1995 .

[9]  Jeffrey Park,et al.  Hunting for azimuthal anisotropy beneath the Pacific Ocean region , 1994 .

[10]  S. Newman,et al.  The role of water in the petrogenesis of Mariana trough magmas , 1994 .

[11]  D. Forsyth,et al.  Seismic anisotropy in the mantle beneath an oceanic spreading centre , 1993, Nature.

[12]  C. Langmuir,et al.  Effects of the melting regime on the composition of the oceanic crust , 1992 .

[13]  J. Gerald,et al.  Seismic wave dispersion and attenuation in Åheim dunite: an experimental study , 1992 .

[14]  T. Jordan,et al.  Mantle layering from ScS reverberations: 3. The upper mantle , 1991 .

[15]  Jean-Paul Montagner,et al.  Global upper mantle tomography of seismic velocities and anisotropies , 1991 .

[16]  S. Karato,et al.  Defect microdynamics in minerals and solid state mechanisms of seismic wave attenuation and velocity dispersion in the mantle , 1990 .

[17]  S. Karato,et al.  The role of hydrogen in the electrical conductivity of the upper mantle , 1990, Nature.

[18]  T. Murase,et al.  Qp‐melting temperature relation in peridotite at high pressure and temperature: Attenuation mechanism and implications for the mechanical properties of the upper mantle , 1989 .

[19]  D. Stevenson,et al.  A self‐consistent model of melting, magma migration and buoyancy‐driven circulation beneath mid‐ocean ridges , 1989 .

[20]  M. Bickle,et al.  The Volume and Composition of Melt Generated by Extension of the Lithosphere , 1988 .

[21]  S. Galer,et al.  Magmagenesis and the mapping of chemical and isotopic variations in the mantle , 1986 .

[22]  M. Paterson,et al.  Rheology of synthetic olivine aggregates: Influence of grain size and water , 1986 .

[23]  S. Karato Does partial melting reduce the creep strength of the upper mantle? , 1986, Nature.

[24]  H. Schmeling,et al.  Numerical models on the influence of partial melt on elastic, anelastic and electric properties of rocks. Part I: elasticity and anelasticity , 1985 .

[25]  D. L. Anderson,et al.  Mapping convection in the mantle , 1984 .

[26]  M. Ólafsson,et al.  Phase relations of amphibole, amphibole-carbonate, and phlogopite-carbonate peridotite: petrologic constraints on the asthenosphere , 1983 .

[27]  E. Aulbach,et al.  Shear modulus and Q of forsterite and dunite near partial melting from forced-oscillation experiments , 1982 .

[28]  M. Kumazawa,et al.  Melting of forsterite Mg2SiO4 up to 15 GPa , 1981 .

[29]  T. Shankland,et al.  Geophysical Constraints on Partial Melt in the Upper Mantle (Paper 1R0664) , 1981 .

[30]  D. L. Anderson,et al.  Preliminary reference earth model , 1981 .

[31]  D. Anderson,et al.  A model of dislocation-controlled rheology for the mantle , 1981, Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences.

[32]  R. Evans,et al.  Halogens in the mantle beneath the North Atlantic , 1980, Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences.

[33]  Y. Bottinga,et al.  A geophysical, geochemical, petrological model of the sub-marine lithosphere , 1979 .

[34]  D. Forsyth The evolution of the upper mantle beneath mid-ocean ridges☆ , 1977 .

[35]  B. Parsons,et al.  An analysis of the variation of ocean floor bathymetry and heat flow with age , 1977 .

[36]  H. D. Garbin,et al.  Elastic moduli of a medium with liquid-filled cracks , 1975 .

[37]  T. Yoshii Regionality of group velocities of Rayleigh waves in the Pacific and thickening of the plate , 1975 .

[38]  Y. Guéguen,et al.  High attenuation and the low-velocity zone , 1973 .

[39]  D. Shaw Trace element fractionation during anatexis , 1970 .

[40]  Mineo Kumazawa,et al.  Elastic moduli, pressure derivatives, and temperature derivatives of single‐crystal olivine and single‐crystal forsterite , 1969 .

[41]  Don L. Anderson,et al.  The Effect of Temperature and Partial Melting on Velocity and Attenuation in a Simple Binary System , 1968 .

[42]  D. McKenzie Some remarks on heat flow and gravity anomalies , 1967 .

[43]  H. Keppler,et al.  Solubility of water in the α, β and γ phases of (Mg,Fe)2SiO4 , 1996 .

[44]  S. Karato Effects of Water on Seismic Wave Velocities in the Upper Mantle , 1995 .

[45]  J. Sinton,et al.  Mantle Flow and Melt Generation at Mid-Ocean Ridges , 1992 .

[46]  C. Langmuir,et al.  Petrological systematics of mid-ocean ridge basalts: Constraints on melt generation beneath ocean ridges , 1992 .

[47]  A. Ringwood Composition and petrology of the earth's mantle , 1975 .

[48]  D. L. Anderson,et al.  Partial melting in the upper mantle , 1970 .