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Bea, F., Arzamastsev, A., Montero, P., Arzamastseva, L. (2001) Anomalous alkaline rocks of Soustov, Kola: evidence of mantle-derived metasomatic fluids affecting crustal materials. Contributions to Mineralogy and Petrology, 140 (5) 554-566 doi:10.1007/s004100000211

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Reference TypeJournal (article/letter/editorial)
TitleAnomalous alkaline rocks of Soustov, Kola: evidence of mantle-derived metasomatic fluids affecting crustal materials
JournalContributions to Mineralogy and Petrology
AuthorsBea, F.Author
Arzamastsev, A.Author
Montero, P.Author
Arzamastseva, L.Author
Year2001 (February)Volume140
Issue5
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s004100000211Search in ResearchGate
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Mindat Ref. ID77980Long-form Identifiermindat:1:5:77980:3
GUID0
Full ReferenceBea, F., Arzamastsev, A., Montero, P., Arzamastseva, L. (2001) Anomalous alkaline rocks of Soustov, Kola: evidence of mantle-derived metasomatic fluids affecting crustal materials. Contributions to Mineralogy and Petrology, 140 (5) 554-566 doi:10.1007/s004100000211
Plain TextBea, F., Arzamastsev, A., Montero, P., Arzamastseva, L. (2001) Anomalous alkaline rocks of Soustov, Kola: evidence of mantle-derived metasomatic fluids affecting crustal materials. Contributions to Mineralogy and Petrology, 140 (5) 554-566 doi:10.1007/s004100000211
In(2001, February) Contributions to Mineralogy and Petrology Vol. 140 (5) Springer Science and Business Media LLC

See Also

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Bea, F., Arzamastsev, A., Montero, P., & Arzamastseva, L. (2001). Anomalous alkaline rocks of Soustov, Kola: evidence of mantle-derived metasomatic fluids affecting crustal materials. Contributions to Mineralogy and Petrology, 140(5), 554-566.
Arzamastsev, A. A., Bea, F., Arzamastseva, L. V., Montero, P. (2006) Proterozoic Gremyakha-Vyrmes Polyphase Massif, Kola Peninsula: An example of mixing basic and alkaline mantle melts. Petrology, 14 (4) 361-389 doi:10.1134/s0869591106040035
Arzamastsev, A. A., Glaznev, V. N., Arzamastseva, L. V., Bea, F., Montero, P. (2001) Kola alkaline province in the Paleozoic: evaluation of primary mantle magma composition and magma generation conditions. Russian Journal of Earth Sciences, 3 (1) 1-32 doi:10.2205/2001es000054
Arzamastsev, A. A., Arzamastseva, L. V., Bea, F., Montero, P. (2002) Rare earth elements in rocks and minerals from alkaline plutons of the Kola Peninsula, NW Russia, as indicators of alkaline magma evolution. Russian Journal of Earth Sciences, 4 (3) 187-209 doi:10.2205/2002es000094
Arzamastsev, A. A., Arzamastseva, L. V., Bea, F., Montero, P. (2009) Trace elements in minerals as indicators of the evolution of alkaline ultrabasic dike series: LA-ICP-MS data for the magmatic provinces of northeastern Fennoscandia and Germany. Petrology, 17 (1) 46-72 doi:10.1134/s0869591109010032
Arzamastsev, A. A., Montero, P., Travin, A. V., Arzamastseva, L. V., Bea, F., Fedotov, Zh. A. (2006) Evidence for Sveconorwegian (Grenvillian) magmatic activity in the Northwestern Baltic Shield. Doklady Earth Sciences, 410 (1) 1034-1037 doi:10.1134/s1028334x06070075
Stalder, R., Ulmer, P., Thompson, A., Günther, D. (2001) High pressure fluids in the system MgO–SiO2–H2O under upper mantle conditions. Contributions to Mineralogy and Petrology, 140 (5) 607-618 doi:10.1007/s004100000212
Mayer, B., Jung, S., Brauns, M., Münker, C. (2018) The role of mantle-hybridization and crustal contamination in the petrogenesis of lithospheric mantle-derived alkaline rocks: constraints from Os and Hf isotopes. Contributions to Mineralogy and Petrology, 173 (6) doi:10.1007/s00410-018-1473-2
Zinngrebe, E., Foley, S. F. (1995) Metasomatism in mantle xenoliths from Gees, West Eifel, Germany: evidence for the genesis of calc-alkaline glasses and metasomatic Ca-enrichment. Contributions to Mineralogy and Petrology, 122 (1) 79-96 doi:10.1007/s004100050114
Kozlov, E. N., Arzamastsev, A. A. (2015) Petrogenesis of metasomatic rocks in the fenitized zones of the Ozernaya Varaka alkaline ultrabasic complex, Kola Peninsula. Petrology, 23 (1) 45-67 doi:10.1134/s0869591115010026
Glassley, William E. (1983) Deep crustal carbonates as CO2 fluid sources: Evidence from metasomatic reaction zones. Contributions to Mineralogy and Petrology, 84 (1) 15-24 doi:10.1007/bf01132326
 
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