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Wolf, M. B., Wyllie, P. J. (1991) Dehydration-melting of solid amphibolite at 10 kbar: Textural development, liquid interconnectivity and applications to the segregation of magmas. Mineralogy and Petrology, 44 (3) 151-179 doi:10.1007/bf01166961

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Reference TypeJournal (article/letter/editorial)
TitleDehydration-melting of solid amphibolite at 10 kbar: Textural development, liquid interconnectivity and applications to the segregation of magmas
JournalMineralogy and Petrology
AuthorsWolf, M. B.Author
Wyllie, P. J.Author
Year1991Volume44
Issue3
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/bf01166961Search in ResearchGate
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Mindat Ref. ID15871Long-form Identifiermindat:1:5:15871:8
GUID0
Full ReferenceWolf, M. B., Wyllie, P. J. (1991) Dehydration-melting of solid amphibolite at 10 kbar: Textural development, liquid interconnectivity and applications to the segregation of magmas. Mineralogy and Petrology, 44 (3) 151-179 doi:10.1007/bf01166961
Plain TextWolf, M. B., Wyllie, P. J. (1991) Dehydration-melting of solid amphibolite at 10 kbar: Textural development, liquid interconnectivity and applications to the segregation of magmas. Mineralogy and Petrology, 44 (3) 151-179 doi:10.1007/bf01166961
In(1991) Mineralogy and Petrology Vol. 44 (3) Springer Science and Business Media LLC

See Also

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Wolf, Michael B., Wyllie, Peter J. (1994) Dehydration-melting of amphibolite at 10 kbar: the effects of temperature and time. Contributions to Mineralogy and Petrology, 115 (4) 369-383 doi:10.1007/bf00320972
Wolf, Michael B., Wyllie, Peter J. (1995) Liquid segregation parameters from amphibolite dehydration melting experiments. Journal of Geophysical Research: Solid Earth, 100. 15611-15621 doi:10.1029/95jb00660
Johnston, A. Dana, Wyllie, Peter J. (1988) Interaction of granitic and basic magmas: experimental observations on contamination processes at 10 kbar with H2O. Contributions to Mineralogy and Petrology, 98 (3) 352-362 doi:10.1007/bf00375185
Sekine, T., Wyllie, P. J. (1982) The system granite-peridotite-H2O at 30 kbar, with applications to hybridization in subduction zone magmatism. Contributions to Mineralogy and Petrology, 81 (3) 190-202 doi:10.1007/bf00371296
PATI O DOUCE, A. E., BEARD, J. S. (1995) Dehydration-melting of Biotite Gneiss and Quartz Amphibolite from 3 to 15 kbar. Journal of Petrology, 36 (3) 707-738 doi:10.1093/petrology/36.3.707
Rutter, Michael J., Wyllie, Peter J. (1988) Melting of vapour-absent tonalite at 10 kbar to simulate dehydration–melting in the deep crust. Nature, 331 (6152). 159-160 doi:10.1038/331159a0
Johnston, A. Dana, Wyllie, Peter J. (1989) The system tonalite-peridotite-H2O at 30 kbar, with applications to hybridization in subduction zone magmatism. Contributions to Mineralogy and Petrology, 102 (3) 257-264 doi:10.1007/bf00373719
Lee, W. J., Wyllie, P. J. (2000) The system CaO-MgO-SiO2-CO2 at 1 GPa, metasomatic wehrlites, and primary carbonatite magmas. Contributions to Mineralogy and Petrology, 138 (3) 214-228 doi:10.1007/s004100050558
Huang, W. L., Wyllie, P. J. (1973) Melting relations of muscovite-granite to 35 kbar as a model for fusion of metamorphosed subducted oceanic sediments. Contributions to Mineralogy and Petrology, 42 (1) 1-14 doi:10.1007/bf00521643
Sen, Cuneyt, Dunn, Todd (1994) Dehydration melting of a basaltic composition amphibolite at 1.5 and 2.0 GPa: implications for the origin of adakites. Contributions to Mineralogy and Petrology, 117 (4) 394-409 doi:10.1007/bf00307273
Bertka, Constance M., Holloway, John R. (1994) Anhydrous partial melting of an iron-rich mantle I: subsolidus phase assemblages and partial melting phase relations at 10 to 30 kbar. Contributions to Mineralogy and Petrology, 115 (3) 313-322 doi:10.1007/bf00310770
 
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