The partitioning of Fe and Mg between olivine and carbonate and the stability of carbonate under mantle conditions
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- Type
- article
- Published
- 1993-09-01
- Cited by
- 69
- References
- 45
- OpenAlex
- https://openalex.org/W2085882555
- Semantic Scholar
- https://api.semanticscholar.org/CorpusID:129058950
Keywords
Magnesite, Olivine, Dolomite, Carbonate, Calcite
References
- The formation of pigeonite on the join hedenbergite-ferrosilite at 11.5 and 15 kbar; experiments and a solution model
- Melting of a dry peridotite at high pressures and basalt magma genesis
- An equation of state for carbon dioxide to high pressure and temperature
- An internally consistent dataset with uncertainties and correlations: 3. Applications to geobarometry, worked examples and a computer program
- Experimental determination of activities in Fe−Mg olivine at 1400 K
- Evidence for carbonate in the mantle
- An enlarged and updated internally consistent thermodynamic dataset with uncertainties and correlations: the system K2O–Na2O–CaO–MgO–MnO–FeO–Fe2O3–Al2O3–TiO2–SiO2–C–H2–O2
- Carbonation of peridotites and decarbonation of siliceous dolomites represented in the system CaO-MgO-SiO2-CO2 to 30 kbar
- The solidus of carbonated, fertile peridotite
- Carbonate-silicate reactions at high presures and possible presence of dolomite and magnesite in the upper mantle
- An experimental study of Fe-Mg partitioning between garnet and olivine and its calibration as a geothermometer
- Solidus reactions in synthetic lherzolite-H2O-CO2 from 20–30 kbar, with applications to melting and metasomatism
- Garnet-orthopyroxene and orthopyroxene-clinopyroxene relationships in simple and complex systems
- Pyroxene-carbonate reactions in the upper mantle
- Does CO2 cause partial melting in the low-velocity layer of the mantle?
- Vesicularity and CO2 in mid-ocean ridge basalt
- Phase relations in peridotite+CO2 Systems to 12 GPa: Implications for the origin of kimberlite and carbonate stability in the Earth's upper mantle
- Abundance and distribution of water, carbon and sulfur in the glassy rims of submarine pillow basalts
- Thermodynamic analyses of equilibria involving olivine, orthopyroxene and garnet
- Mantle Fluid Compositions Buffered in Peridotite-CO2-H2O by Carbonates, Amphibole, and Phlogopite
Cited by
- Recyclage du carbone et formation du diamant en zone de subduction : contraintes expérimentales
- Redox - pressure - temperature conditions in the continental upper mantle in relation to C-O-H fluid speciation
- Olivine from the Pionerskaya and V. Grib kimberlite pipes, Arkhangelsk diamond province, Russia: Types, composition, and origin
- An internally consistent thermodynamic data set for phases of petrological interest
- No slab‐derived CO2 in Mariana Trough back‐arc basalts: Implications for carbon subduction and for temporary storage of CO2 beneath slow spreading ridges
- Electron microprobe analysis of geological carbonates
- Experimental determination of the reaction dolomite + 2 coesite = diopside + 2 CO2 to 6 GPa
- Carbonate inclusions in Lower Cretaceous picrites from the Hončova hůrka Hill (Czech Republic, Outer Western Carpathians): Evidence for primary magmatic carbonates?
- Oxygen fugacity of the diamond + CO fluid assemblage and CO2 fugacity at 8 GPa
- Experimental petrology of upper mantle materials, processes and products
- Experimental investigation of silicate-carbonate system at high pressure and high temperature
- Carbonate-silicate equilibria in the high-magnesia ultrapotassic volcanics of the Toro-Ankole Province (Eastern African rift zone)
- Diamond formation and source carbonation: mineral associations in diamonds from Namibia
- Origin of Group 1A kimberlites: Fluid-saturated melting experiments at 45–55 kbar
- Carbonatitic melts along the solidus of model lherzolite in the system CaO-MgO-Al2O3-SiO2-CO2 from 3 to 7 GPa
- Significance of silicate melt pockets in upper mantle xenoliths from the Bakony-Balaton Highland Volcanic Field, Western Hungary
- Petrogenesis of the melilititic and nephelinitic rock suites in the Lake Natron–Engaruka monogenetic volcanic field, northern Tanzania
- How unique is the Udachnaya-East kimberlite? Comparison with kimberlites from the Slave Craton (Canada) and SW Greenland
- Mineral equilibria of diamond-forming carbonate-silicate systems
- Modification of the subcontinental mantle beneath East Serbia: evidence from orthopyroxene-rich xenoliths
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