Browsing by Author "Rabinowicz M."
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Browsing by Author "Rabinowicz M."
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Rabinowicz M.; Genthon P.; Ceuleneer G.; Hillairet M. (2001)Most compaction models in the partially molten mantle have addressed the case of low intergranular melt concentrations (up to a few percent). Here we develop a mathematical and numerical formalism adapted to the two-dimensional ...
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Dubuffet F.; Yuen D.A.; Rabinowicz M. (1999)A physical model describing the temperature and pressure dependences of mantle thermal conductivity has recently been provided by A.M. Hofmeister [Science 283 (1999) 1699-1706]. We have studied numerically the influences ...
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Cserepes L.; Rabinowicz M. (1985)One of the current models of mantle convection assumes that the circulation takes place in two superimposed layers separated by the 700-km discontinuity. The present study reports two-dimensional numerical experiments ...
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Gregoire M.; Rabinowicz M.; Janse A.J.A. (2006)Kimberlite pipes or dykes tend to occur in clusters (a few kilometres in diameter) within fields ?30–50?km in diameter. They are generally considered to originate from low degrees of partial melting of carbonated peridotite ...
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Khodakovskii G.; Rabinowicz M.; Ceuleneer G.; Trubitsyn V.P. (1995)Data collected in ophiolite massifs indicate that some horizons with very high melt fractions have been frozen during the accretion of the harzburgites just below the crust. We show that the existence, distribution and ...
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Dubuffet F.; Rabinowicz M.; Monnereau M. (2000)The multiple-scales structure of mantle convection remains largely unknown. A 3D model of convection is used to investigate the effect of a viscosity step on the multiple-scales pattern of an infinite Prandtl number ...
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Fontaine F.J.; Rabinowicz M.; Boulegue J. (2001)The hydrothermal processes at ridge crests have been extensively studied during the last two decades. Nevertheless, the reasons why hydrothermal fields are only occasionally found along some ridge segments remain a matter ...
Now showing items 1-7 of 7