Some Remarks on Melting and Extreme Metamorphism of Crustal Rocks (original) (raw)

Experiments on the kinetics of partial melting of a leucogranite at 200 MPa H2O and 690–800°C: compositional variability of melts during the onset of H2O-saturated crustal anatexis

Antonio Acosta-vigil

Contributions to Mineralogy and Petrology, 2006

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An experimental study of grain scale melt segregation mechanisms in two common crustal rock types

Tracy Rushmer

Journal of Metamorphic Geology, 2002

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Volume change during partial melting reactions: implications for melt extraction, melt geochemistry and crustal rheology

Tracy Rushmer

Tectonophysics, 2001

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Accessory phase controls on the geochemistry of crustal melts and restites produced during water-undersaturated partial melting

Simon Harley

Contributions to Mineralogy and Petrology, 1993

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Slab melting versus slab dehydration in subduction-zone magmatism

Tatsuhiko Kawamoto, Shigeaki Ono

Proceedings of the …, 2011

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Experimental and theoretical constraints on melt distribution in crustal sources: the effect of crystalline anisotropy on melt interconnectivity

Didier Laporte

Chemical Geology, 1995

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Wetting behavior of partial melts during crustal anatexis: the distribution of hydrous silicic melts in polycrystalline aggregates of quartz

Didier Laporte

Contributions to Mineralogy and Petrology, 1994

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Melt extraction and accumulation from partially molten rocks

Alvar Soesoo

Lithos, 2004

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Recovering the composition of melt and the fluid regime at the onset of crustal anatexis and S-type granite formation

Sandro Meli

Geology, 2013

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Stability of hydrous melt at the base of the Earth's upper mantle

Eiji Ohtani

Nature, 2006

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Comment on ‘‘The beginnings of hydrous mantle wedge melting’’, CB Till, TL Grove, AC Withers, Contributions to Mineralogy and Petrology, DOI 10.1007/s00410-011-0692-6

Istvan Kovacs

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Thermodynamics of minerals and melts

Mark Ghiorso

Rev Geophys, 1991

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Experimental Study of the Influence of Water on Melting and Phase Assemblages in the Upper Mantle

Trevor Falloon

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Monazite control on Th, U and REE redistribution during partial melting: experiment and application to the deeply subducted crust

Aleksandr Stepanov

2012

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Dehydration melting of tonalites. Part II. Composition of melts and solids

Dr JAIKARAN SINGH

Contributions to Mineralogy and Petrology, 1996

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Kinetics of melt migration in upper mantle-type rocks

David Kohlstedt

Earth and Planetary Science Letters, 1991

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Experimental melting of biotite+plagioclase+quartz+/-muscovite assemblages and implications for crustal melting

Véronique Gardien

Journal of Geophysical Research, 1995

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Effects of pressure and H2O content on the compositions of primary crustal melts

Alberto Patino Douce

Earth and Environmental Science Transactions of the Royal Society of Edinburgh, 1996

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Formation of a high-temperature metamorphic complex due to pervasive melt migration in the hot crust

Kazuhiro Miyazaki

Island Arc, 2007

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Supercooled melt inclusions in lower-crustal granulites as a consequence of rapid exhumation by channel flow

Satish-Kumar M.

Gondwana Research, 2014

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Rey etal 2011 Geology-SupMat

Patrice F Rey

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Dehydration melting and the relationship between granites and granulites

Leonid Aranovich

Precambrian Research, 2014

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Strain heating as a mechanism for partial melting and ultrahigh temperature metamorphism in convergent orogens: Implications of temperature-dependent thermal diffusivity and rheology

Alan Whittington

Journal of Geophysical Research, 2010

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Rheological Transitions During Partial Melting and Crystallization with Application to Felsic Magma Segregation and Transfer

CUNEY Michel

Journal of Petrology, 1996

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Melt Segregation From Partially Molten Source Regions: the Importance of Melt Density and Source Region Size

Bradford Hager

Journal of Geophysical …, 1981

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Role of melt during deformation in the deep crust

Lincoln Hollister

Terra Nova, 1994

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Partial melting of metagreywacke: a calculated mineral equilibria study

Tim Johnson

Journal of Metamorphic Geology, 2008

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Transforming mylonitic metagranite by open‐system interactions during melt flow

Ondrej Lexa

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Melting of Refractory Mantle at 1middle dot5, 2 and 2middle dot5 GPa under Anhydrous and H2O-undersaturated Conditions: Implications for the Petrogenesis of High-Ca Boninites and the Influence of Subduction Components on Mantle Melting

Trevor Falloon

J Petrol, 2000

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Experimental tests of low degree peridotite partial melt compositions: implications for the nature of anhydrous near-solidus peridotite melts at 1 GPa. Earth Planet Sci Lett

Trevor Falloon

Earth and Planetary Science Letters

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Experimental tests of low degree peridotite partial melt compositions: implications for the nature of anhydrous near-solidus peridotite melts at 1 GPa

Trevor Falloon

Earth and Planetary Science Letters, 1997

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Fluid-absent Melting of High-grade Semi-pelites: P-T Constraints on Orthopyroxene Formation and Implications for Granulite Genesis

Thomas Chacko

Journal of Petrology, 2002

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Crystallization calculations for a binary melt cooling at constant rates of heat removal: implications for the crystallization of magma bodies

T. Spohn

Earth and Planetary Science Letters, 1991

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An analysis of variations in isentropic melt productivity

Paul Asimow

Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 1997

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NATURE | VOL 408 | 7 DECEMBER 2000 | www Granite magma formation, transport and emplacement in the Earth's crust

jean louis

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