Segregation of subducted oceanic crust in the convecting mantle
暂无分享,去创建一个
[1] H. Nataf,et al. SEISMIC DISCONTINUITY AT THE TOP OF D : A WORLD-WIDE FEATURE ? , 1993 .
[2] M. Weber. P- and S-wave reflections from anomalies in the lowermost mantle , 1993 .
[3] D. Yuen,et al. Dynamical consequences of depth-dependent thermal expansivity and viscosity on mantle circulations and thermal structure , 1993 .
[4] David J. Stevenson,et al. Effects of an endothermic phase transition at 670 km depth in a spherical model of convection in the Earth's mantle , 1993, Nature.
[5] R. Boehler,et al. Thermal expansivity in the lower mantle , 1992 .
[6] M. Weber,et al. A search for anomalies in the lowermost mantle using seismic bulletins , 1992 .
[7] H. Nataf,et al. Further evidence for the ‘Lay discontinuity’ beneath northern Siberia and the North Atlantic from short-period P-waves recorded in France , 1992 .
[8] R. Boehler. Melting of the FeFeO and the FeFeS systems at high pressure: Constraints on core temperatures , 1992 .
[9] A. Hofmann,et al. himu-em: The French Polynesian connection , 1992 .
[10] Masayuki Obayashi,et al. Subducting slabs stagnant in the mantle transition zone , 1992 .
[11] U. R. Christensen,et al. An Eulerian technique for thermomechanical modeling of lithospheric extension , 1992 .
[12] T. Jordan,et al. Mantle layering from ScS reverberations: 4. The lower mantle and core-mantle boundary , 1991 .
[13] Guust Nolet,et al. Tomographic imaging of subducted lithosphere below northwest Pacific island arcs , 1991, Nature.
[14] T. Jordan,et al. Seismic strain rate and deep slab deformation in Tonga , 1991 .
[15] B. Weaver. The origin of ocean island basalt end-member compositions: trace element and isotopic constraints , 1991 .
[16] H. Mao,et al. Effect of pressure, temperature, and composition on lattice parameters and density of (Fe,Mg)SiO3‐perovskites to 30 GPa , 1991 .
[17] P. Olson,et al. Experiments on the interaction of thermal convection and compositional layering at the base of the mantle , 1991 .
[18] Patrice Weber,et al. Intermittent layered convection in a model mantle with an endothermic phase change at 670 km , 1991, Nature.
[19] Yusheng Zhao,et al. Phase Transition and Thermal Expansion of MgSiO3 Perovskite , 1991, Science.
[20] M. Weber,et al. Evidence of a laterally variable lower mantle structure from P‐ and S‐waves , 1990 .
[21] R. Clayton,et al. P and S wave travel time inversions for subducting slab under the island arcs of the northwest Pacific , 1990 .
[22] A. Chopelas. Thermal expansion, heat capacity, and entropy of MgO at mantle pressures , 1990 .
[23] T. Tanimoto. Long-wavelength S-wave velocity structure throughout the mantle , 1990 .
[24] Louise H. Kellogg,et al. Mixing and the distribution of heterogeneities in a chaotically convecting mantle , 1990 .
[25] H. Mao,et al. Stability and equation of state of CaSiO3‐Perovskite to 134 GPa , 1989 .
[26] A. E. Ringwood,et al. Slab-mantle interactions , 1989 .
[27] Ulrich R. Christensen,et al. Mixing by time-dependent convection , 1989 .
[28] R. Boehler,et al. Thermal expansion measurements at very high pressure, systematics, and a case for a chemically homog , 1989 .
[29] M. Richards,et al. On the separation of relatively buoyant components from subducted lithosphere , 1989 .
[30] B. Hager,et al. Long-wavelength variations in Earth’s geoid: physical models and dynamical implications , 1989, Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences.
[31] U. Christensen. Models of mantle convection: one or several layers , 1989, Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences.
[32] R. Jeanloz,et al. Simulating the core‐mantle boundary: An experimental study of high‐pressure reactions between silicates and liquid iron , 1989 .
[33] D. Yuen,et al. Dynamical influences from thermal‐chemical instabilities at the core‐mantle boundary , 1989 .
[34] H. Mao,et al. Bulk moduli of magnesiowüstites from static compression measurements , 1989 .
[35] D. L. Anderson,et al. Seismic velocities in mantle minerals and the mineralogy of the upper mantle , 1989 .
[36] U. Christensen. Is subducted lithosphere trapped at the 670-km discontinuity? , 1988, Nature.
[37] N. Sleep. Gradual entrainment of a chemical layer at the base of the mantle by overlying convection , 1988 .
[38] Albrecht W. Hofmann,et al. Chemical differentiation of the Earth: the relationship between mantle, continental crust, and oceanic crust , 1988 .
[39] F. Guyot,et al. X-ray microanalysis of high-pressure/high-temperature phases synthesized from natural olivine in a diamond-anvil cell , 1988 .
[40] David A. Yuen,et al. Numerical simulations of thermal-chemical instabilities at the core–mantle boundary , 1988, Nature.
[41] M. Bickle,et al. The Volume and Composition of Melt Generated by Extension of the Lithosphere , 1988 .
[42] A. E. Ringwood,et al. Nature of the 650–km seismic discontinuity: implications for mantle dynamics and differentiation , 1988, Nature.
[43] C. Young,et al. Evidence for a shear velocity discontinuity in the lower mantle beneath India and the Indian Ocean , 1987 .
[44] M. Gurnis,et al. Interaction of mantle dregs with convection: Lateral heterogeneity at the core‐mantle boundary , 1986 .
[45] H. Newsom,et al. Siderophile and chalcophile element abundances in oceanic basalts, Pb isotope evolution and growth of the Earth's core , 1986 .
[46] M. Gurnis. THE EFFECTS OF CHEMICAL DENSITY DIFFERENCES ON CONVECTIVE MIXING IN THE EARTH'S MANTLE , 1986 .
[47] Donald L. Turcotte,et al. Implications of a two-component marble-cake mantle , 1986, Nature.
[48] M. Gurnis,et al. Mixing in numerical models of mantle convection incorporating plate kinematics , 1986 .
[49] Raymond Jeanloz,et al. Hydrostatic compression of Fe1‐x O Wüstite , 1986 .
[50] F. Albarède,et al. Hydrothermal uranium uptake at ridge crests , 1985, Nature.
[51] N. Hoffman,et al. The destruction of geochemical heterogeneities by differential fluid motions during mantle convection , 1985 .
[52] D. Turcotte. Geodynamic mixing in the mesosphere boundary layer and the origin of oceanic islands: Geophysical Re , 1985 .
[53] W. White. Sources of oceanic basalts: Radiogenic isotopic evidence , 1985 .
[54] D. Yuen,et al. The interaction of a subducting lithospheric slab with a chemical or phase boundary , 1984 .
[55] U. Christensen. Instability of a hot boundary layer and initiation of thermo-chemical plumes , 1984 .
[56] David A. Yuen,et al. Mixing of passive heterogeneities by mantle convection , 1984 .
[57] D. McKenzie,et al. Mantle reservoirs and ocean island basalts , 1983, Nature.
[58] A. E. Ringwood,et al. Phase Transformations and Differentiation in Subducted Lithosphere: Implications for Mantle Dynamics, Basalt Petrogenesis, and Crustal Evolution , 1982, The Journal of Geology.
[59] S. Goldstein,et al. Nd, Sr and Pb isotopic systematics in a three-component mantle: a new perspective , 1982, Nature.
[60] A. Hofmann,et al. Sr and Nd isotope geochemistry of oceanic basalts and mantle evolution , 1982, Nature.
[61] Albrecht W. Hofmann,et al. Mantle plumes from ancient oceanic crust , 1982 .
[62] C. G. Chase. Oceanic island Pb: Two-stage histories and mantle evolution , 1981 .
[63] B. Dupré,et al. Isotopic and chemical effects produced in a continuously differentiating convecting Earth mantle , 1980, Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences.
[64] U. Christensen. The influence of phase transitions and chemical heterogeneity on mantle convection , 1991 .
[65] Steven M. Hein,et al. Computer simulation of Pb and Sr isotope evolution of the Earth's crust and upper mantle , 1973 .