Low-pressure (> 4 MPa) and high-temperature (> 1250 °C) incongruent melting of marly limestone: formation of carbonate melt and melilite–nepheline paralava in the Khamaryn–Khural–Khiid combustion metamorphic complex, East Mongolia

I. S. Peretyazhko, Е. A. Savina, Е. А. Khromova

2021Contributions to Mineralogy and Petrology22 citationsDOI

Topics & Concepts

MeliliteGeologyNephelineGeochemistrySilicateSilicate mineralsMineralogyForsteriteCarbonateChemistrySpinelOrganic chemistryPaleontologyGeological and Geochemical AnalysisHigh-pressure geophysics and materialsearthquake and tectonic studies

Low-pressure (&gt; 4 MPa) and high-temperature (&gt; 1250 °C) incongruent melting of marly limestone: formation of carbonate melt and melilite–nepheline paralava in the Khamaryn–Khural–Khiid combustion metamorphic complex, East Mongolia

Topics & Concepts

Low-pressure (> 4 MPa) and high-temperature (> 1250 °C) incongruent melting of marly limestone: formation of carbonate melt and melilite–nepheline paralava in the Khamaryn–Khural–Khiid combustion metamorphic complex, East Mongolia