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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
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TN_cdi_proquest_journals_2517674497
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https://collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2517674497
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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
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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
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Berlin/Heidelberg: Springer Berlin Heidelberg
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English
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TN_cdi_proquest_journals_2517674497
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https://collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2517674497