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Bridging the gap between subduction dynamics and the long-term strength of the Sunda megathrust. [PDF]
Capitanio FA +6 more
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Cenozoic evolution of earth's strongest geoid low illuminates mantle dynamics beneath Antarctica. [PDF]
Glišović P, Forte AM.
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Rheology of the Upper Mantle: A Synthesis
Science, 1993Rheological properties of the upper mantle of the Earth play an important role in the dynamics of the lithosphere and asthenosphere. However, such fundamental issues as the dominant mechanisms of flow have not been well resolved. A synthesis of laboratory studies and geophysical and geological observations shows that transitions between diffusion and ...
S-I Karato, Patrick Wu
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Ferropericlase—a lower mantle phase in the upper mantle
Lithos, 2004Experiments on compositions along the join MgO–NaA3+Si2O6 (A=Al, Cr, Fe3+) show that sodium can be incorporated into ferropericlase at upper mantle pressures in amounts commonly found in natural diamond inclusions. These results, combined with the observed mineral parageneses of several diamond inclusion suites, establish firmly that ferropericlase ...
Gerhard P Brey +2 more
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Calcium isotope fractionation during magmatic processes in the upper mantle
Geochimica et Cosmochimica Acta, 2019The Earth’s mantle has a complex history of partial melting and melt-peridotite reaction that have redistributed Ca and other elements between residues and melting products.
Chunfei Chen +6 more
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On the seismic discontinuities in the upper mantle
Physics of the Earth and Planetary Interiors, 1995Abstract Mode conversions and reflections at upper-mantle seismic discontinuities may be contained in earthquake seismograms as weak secondary phases that often become visible only after special signal processing techniques are applied to the data. To extract fully the information these secondary phases carry about the three-dimensional structure of ...
Bock, G. +7 more
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Metal saturation in the upper mantle
Nature, 2007The oxygen fugacity f(O2)of the Earth's mantle is one of the fundamental variables in mantle petrology. Through ferric-ferrous iron and carbon-hydrogen-oxygen equilibria, f(O2) influences the pressure-temperature positions of mantle solidi and compositions of small-degree mantle melts.
Rohrbach, A. +5 more
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Diamond Accumulation in the Upper Mantle
Nature, 1970THE present high gradient of density in the upper mantle provides neutral buoyancy zones in which certain minerals may have been accumulated in the past or to which they may still be migrating. The necessary condition for progressive accumulation in such a zone is that the mineral concerned has opportunities of rising or sinking relative to its ...
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Phase Changes in the Upper Mantle
Science, 1967The C-region of the upper mantle has two transition regions 75 to 90 kilometers thick. In western North America these start at depths of 365 kilometers and 620 kilometers and involve velocity increases of about 9 to 10 percent. The locations of these transition regions, their general shape, and their thicknesses are consistent with, first, the ...
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Tectonophysics, 1965
Abstract All current tectonic hypotheses assign the cause of vertical crustal movements to processes within the earth. Some suppose an expansion and contraction of mantle material, probably caused by physical transitions (polymorphic, phase and electronic) and chemical reactions.
S.I. Subbotin +2 more
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Abstract All current tectonic hypotheses assign the cause of vertical crustal movements to processes within the earth. Some suppose an expansion and contraction of mantle material, probably caused by physical transitions (polymorphic, phase and electronic) and chemical reactions.
S.I. Subbotin +2 more
openaire +1 more source

