Melting of carbonated pelite at 5.5–15.5 GPa: implications for the origin of alkali-rich carbonatites and the deep water and carbon cycles
Authors:
- 7 December 2021
- journal article
- research article
- Published by Springer Nature in Contributions to Mineralogy and Petrology
- Vol. 177 (1) , 1-21
Abstract
No abstract availableKeywords
Funding Information
- National Key Research and Development Program of China (2019YFA0708501)
- National Natural Science Foundation of China (41672036, 40972028)
This publication has 135 references indexed in Scilit:
- Flux of carbonate melt from deeply subducted pelitic sediments: Geophysical and geochemical implications for the source of Central American volcanic arcGeophysical Research Letters, 2012
- Solidus and phase relations of carbonated peridotite in the system CaO–Al2O3–MgO–SiO2–Na2O–CO2 to the lower mantle depthsPhysics of the Earth and Planetary Interiors, 2009
- Phase relations of CaAl4Si2O11 at high-pressure and high-temperature with implications for subducted continental crust into the deep mantlePhysics of the Earth and Planetary Interiors, 2008
- The role of mantle ultrapotassic fluids in diamond formationProceedings of the National Academy of Sciences, 2007
- Water transport into the deep mantle and formation of a hydrous transition zonePhysics of the Earth and Planetary Interiors, 2004
- Mantle solidus: Experimental constraints and the effects of peridotite compositionGeochemistry, Geophysics, Geosystems, 2000
- Melting study of an alkali basalt JB-1 up to 12.5 GPa: behavior of potassium in the deep mantlePhysics of the Earth and Planetary Interiors, 1998
- Decomposition of K-amphibole at high pressures and implications for subduction zone volcanismPhysics of the Earth and Planetary Interiors, 1998
- Thermal and dynamical evolution of the upper mantle in subduction zonesJournal of Geophysical Research, 1997
- H2O transport and release in subduction zones: Experimental constraints on basaltic and andesitic systemsJournal of Geophysical Research, 1995