Melting of carbonated pelite at 5.5–15.5 GPa: implications for the origin of alkali-rich carbonatite...
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
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Publisher
Berlin/Heidelberg: Springer Berlin Heidelberg
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Language
English
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Berlin/Heidelberg: Springer Berlin Heidelberg
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Contents
Melting experiments on a carbonated pelite were performed at 5.5–15.5 GPa, 800–1875 °C using multi-anvil apparatuses to determine the melting phase relations and the P–T stability fields of various phases, which may shed some light on the source of silica-undersaturated magmas and the deep Earth carbon and water cycles. The subsolidus assemblages c...
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Full title
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
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TN_cdi_proquest_journals_2607471499
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2607471499
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ISSN
0010-7999
E-ISSN
1432-0967
DOI
10.1007/s00410-021-01867-5
