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Grassi, Daniele, Schmidt, Max W. (2011) Melting of carbonated pelites at 8–13 GPa: generating K-rich carbonatites for mantle metasomatism. Contributions to Mineralogy and Petrology, 162 (1) 169-191 doi:10.1007/s00410-010-0589-9

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Reference TypeJournal (article/letter/editorial)
TitleMelting of carbonated pelites at 8–13 GPa: generating K-rich carbonatites for mantle metasomatism
JournalContributions to Mineralogy and Petrology
AuthorsGrassi, DanieleAuthor
Schmidt, Max W.Author
Year2011 (July)Volume162
Issue1
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s00410-010-0589-9Search in ResearchGate
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Mindat Ref. ID79192Long-form Identifiermindat:1:5:79192:0
GUID0
Full ReferenceGrassi, Daniele, Schmidt, Max W. (2011) Melting of carbonated pelites at 8–13 GPa: generating K-rich carbonatites for mantle metasomatism. Contributions to Mineralogy and Petrology, 162 (1) 169-191 doi:10.1007/s00410-010-0589-9
Plain TextGrassi, Daniele, Schmidt, Max W. (2011) Melting of carbonated pelites at 8–13 GPa: generating K-rich carbonatites for mantle metasomatism. Contributions to Mineralogy and Petrology, 162 (1) 169-191 doi:10.1007/s00410-010-0589-9
In(2011, July) Contributions to Mineralogy and Petrology Vol. 162 (1) Springer Science and Business Media LLC

See Also

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Grassi, Daniele, Schmidt, Max W. (2011) The Melting of Carbonated Pelites from 70 to 700 km Depth. Journal of Petrology, 52 (4) 765-789 doi:10.1093/petrology/egr002
Thomsen, Tonny B., Schmidt, Max W. (2008) Melting of carbonated pelites at 2.5–5.0 GPa, silicate–carbonatite liquid immiscibility, and potassium–carbon metasomatism of the mantle. Earth and Planetary Science Letters, 267 (1) 17-31 doi:10.1016/j.epsl.2007.11.027
Tsuno, Kyusei, Dasgupta, Rajdeep (2011) Melting phase relation of nominally anhydrous, carbonated pelitic-eclogite at 2.5–3.0 GPa and deep cycling of sedimentary carbon. Contributions to Mineralogy and Petrology, 161 (5) 743-763 doi:10.1007/s00410-010-0560-9
Chen, Xueqian, Wang, Meili, Inoue, Toru, Liu, Qiong, Zhang, Lifei, Bader, Thomas (2022) Correction to: 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. Contributions to Mineralogy and Petrology, 177 (2) doi:10.1007/s00410-022-01886-w
Chen, Xueqian, Wang, Meili, Inoue, Toru, Liu, Qiong, Zhang, Lifei, Bader, Thomas (2022) 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. Contributions to Mineralogy and Petrology, 177 (1) doi:10.1007/s00410-021-01867-5
Chu, Linglin, Enggist, Andreas, Luth, Robert W. (2011) Effect of KCl on melting in the Mg2SiO4–MgSiO3–H2O system at 5 GPa. Contributions to Mineralogy and Petrology, 162 (3) 565-571 doi:10.1007/s00410-011-0612-9
Ghosh, Sujoy, Litasov, Konstantin, Ohtani, Eiji (2014) Phase relations and melting of carbonated peridotite between 10 and 20 GPa: a proxy for alkali- and CO2-rich silicate melts in the deep mantle. Contributions to Mineralogy and Petrology, 167 (2) doi:10.1007/s00410-014-0964-z
Grassi, Daniele, Schmidt, Max W., Günther, Detlef (2012) Element partitioning during carbonated pelite melting at 8, 13 and 22GPa and the sediment signature in the EM mantle components. Earth and Planetary Science Letters, 327. 84-96 doi:10.1016/j.epsl.2012.01.023
Weidendorfer, Daniel, Manning, Craig E., Schmidt, Max W. (2020) Carbonate melts in the hydrous upper mantle. Contributions to Mineralogy and Petrology, 175 (8). doi:10.1007/s00410-020-01708-x
Borghini, G., Fumagalli, P., Rampone, E. (2017) Partial melting of secondary pyroxenite at 1 and 1.5 GPa, and its role in upwelling heterogeneous mantle. Contributions to Mineralogy and Petrology, 172 (8) doi:10.1007/s00410-017-1387-4
Kessel, R., Pettke, T., Fumagalli, P. (2015) Melting of metasomatized peridotite at 4–6 GPa and up to 1200 °C: an experimental approach. Contributions to Mineralogy and Petrology, 169 (4) doi:10.1007/s00410-015-1132-9
 
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