Categories Research article 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 Post author By vlad.ilie Post date May 22, 2022 No Comments on 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 ← Sustainable energy performances of green buildings: A review of current theories implementations and challenges → Impact of household air pollution on human health: source identification and systematic management approach Leave a Reply Cancel replyYour email address will not be published. Required fields are marked *Comment * Name * Email * Website Save my name, email, and website in this browser for the next time I comment. Δ
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