Conditions of magmatic crystallization of Na-bearing majoritic garnets in the earth mantle: Evidence from experimental and natural data (original) (raw)

Phase relations and formation of sodium-rich majoritic garnet in the system Mg3Al2Si3O12–Na2MgSi5O12 at 7.0 and 8.5 GPa

Anna Dymshits

Contributions to Mineralogy and Petrology, 2008

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The Mg 3 Al 2 Si 3 O 12-Na 2 MgSi 5 O 12 system at pressures of 7.0 and 8.5 GPa and a temperature of 1300–1800° C: Phase relationships and crystallization of Na-bearing majoritic garnet

Anna Dymshits

2012

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Na-bearing majoritic garnet in the Na2MgSi5O12–Mg3Al2Si3O12 join at 11–20GPa: Phase relations, structural peculiarities and solid solutions

Luca Bindi, Anton Shatskiy

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Phase relations on the diopside–jadeite–hedenbergite join up to 24GPa and stability of Na-bearing majoritic garnet

Masaki Akaogi

Geochimica et Cosmochimica Acta, 2008

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Experimental study of the pyroxene-garnet phase transition in the Na2MgSi5O12 system at pressures of 13–20 GPa: First synthesis of sodium majorite

Anton Shatskiy

Doklady Earth Sciences, 2010

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Computer simulation of Na-bearing majoritic garnet

Anna Dymshits

Doklady Earth Sciences, 2011

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Partitioning of trace elements between Na-bearing majoritic garnet and melt at 8.5GPa and 1500–1900°C

Teresa Jeffries, Luca Bindi

Lithos, 2014

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A mechanism for Na incorporation in garnet: An example from garnet in orthogneiss from the SuLu terrane, eastern China

Takeyoshi Yoshida

1995

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Crystal chemistry of sodium in the Earth's interior: The structure of Na2MgSi5O12 synthesized at 17.5 GPa and 1700 C

Luca Bindi, Anton Shatskiy

American Mineralogist, 2011

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Generation of highly silicic magmas at ultra-high temperature conditions : evidence from melt inclusions in peritectic garnet

Satish-Kumar M.

2021

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Oriented growth of garnet by topotactic reactions and epitaxy in high-pressure, mafic garnet granulite formed by dehydration melting of metastable hornblende-gabbronorite (Jijal Complex, Kohistan Complex, north Pakistan)

José Alberto Padrón-Navarta

Journal of Metamorphic Geology, 2008

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Compositional change of majoritic garnet in a MORB composition from 7 to 17 GPa and 1400 to 1600°C

Shigeaki Ono

Physics of the Earth and Planetary Interiors, 1996

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Compositional evolution of grossular garnet from leucotonalitic pegmatite at Ruda nad Moravou, Czech Republic; a complex EMPA, LA-ICP-MS, IR and CL study

Milan Novák

Mineralogy and Petrology, 2013

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Garnet and diopside-bearing diamondites (framesites)

Gabor Dobosi

Mineralogy and Petrology, 2000

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Powder X ray diffraction study of synthetic pyrope-grossular garnets between 20 and 295 K

Charles A. Geiger

Journal of Geophysical Research, 1997

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Garnet re-equilibration by coupled dissolution-reprecipitation: evidence from textural, major element and oxygen isotope zoning of ‘cloudy’ garnet

Laure Martin, Olivier Vanderhaeghe

Journal of Metamorphic Geology, 2011

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P–V–T equation of state of Na-majorite to 21GPa and 1673K

Anton Shatskiy

Physics of the Earth and Planetary Interiors, 2014

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Thermal equation of state of garnets along the pyrope-majorite join

Yanbin Wang

Physics of The Earth and Planetary Interiors, 1998

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Melting of hydrous and carbonate mineral inclusions in garnet host during ultrahigh pressure experiments

A. Perchuk

Lithos, 2008

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Modification of mineral inclusions in garnet under high-pressure conditions: experimental simulation and application to the carbonate-silicate rocks of Kokchetav massif

H.-P. Schertl

Russian Geology and Geophysics, 2009

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EPMA Major and Trace Element Analysis in Garnet and its Petrological Application

Alessandro Borghi

Mikrochimica Acta, 2002

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Evidence of majoritic garnet from the mantle transition zone in the Alpe Arami garnet peridotite

Asish Basu

International Geology Review, 2019

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Partitioning of trace elements between garnet, clinopyroxene and diamond-forming carbonate-silicate melt at 7 GPa

F. Wall

Mineralogical Magazine, 2010

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High-pressure crystallization vs. recrystallization origin of garnet pyroxenite-eclogite within subduction related lithologies

Shah Wali Faryad

Mineralogy and Petrology, 2018

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Combined thermodynamic and rare earth element modelling of garnet growth during subduction: Examples from ultrahigh-pressure eclogite of the Western Gneiss …

Dorrit Jacob

Earth and Planetary Science Letters, 2008

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Formation of garnet polycrystals during metamorphic crystallization

Karsten Kunze

Journal of Metamorphic Geology, 2008

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Garnets: Structure, compressibility, dynamics, and disorder

Victor Milman

JOM, 2000

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High-pressure phase equilibria in a garnet lherzolite, with special reference to Mg2+Fe2+ partitioning among constituent minerals

Masaki Akaogi

Physics of the Earth and Planetary Interiors, 1979

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Mantle refertilization by melts of crustal-derived garnet pyroxenite

Jean-Louis Bodinier

HAL (Le Centre pour la Communication Scientifique Directe), 2015

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Precipitation of pyroxenes and Mg2SiO4 from majoritic garnet: simulation of peridotite exhumation from great depth

Larissa Dobrzhinetskaya, Herman van Roermund, Krassimir Bozhilov

Terra Nova, 2004

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Phosphorus – an omnipresent minor element in garnet of diverse textural types from leucocratic granitic rocks

Jan Cempirek

Mineralogy and Petrology, 2005

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