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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

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Reference TypeJournal (article/letter/editorial)
TitleMelting relations of muscovite-granite to 35 kbar as a model for fusion of metamorphosed subducted oceanic sediments
JournalContributions to Mineralogy and Petrology
AuthorsHuang, W. L.Author
Wyllie, P. J.Author
Year1973 (March)Volume42
Issue1
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/bf00521643Search in ResearchGate
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Mindat Ref. ID73908Long-form Identifiermindat:1:5:73908:1
GUID0
Full ReferenceHuang, 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
Plain TextHuang, 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
In(1973, March) Contributions to Mineralogy and Petrology Vol. 42 (1) Springer Science and Business Media LLC

See Also

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Stern, C. R., Wyllie, P. J. (1973) Melting relations of basalt-andesile-rhyolite-H2O and a pelagic red clay at 30 kb. Contributions to Mineralogy and Petrology, 42 (4) 313-323 doi:10.1007/bf00372609
Huang, W.L., Wyllie, P.J. (1973) Muscovite dehydration and melting in deep crust and subducted oceanic sediments. Earth and Planetary Science Letters, 18 (1) 133-136 doi:10.1016/0012-821x(73)90045-9
Huang, W. L., Wyllie, P. J. (1981) Phase relationships of S-type granite with H2O to 35 kbar: Muscovite granite from Harney Peak, South Dakota. Journal of Geophysical Research: Solid Earth, 86. 10515-10529 doi:10.1029/jb086ib11p10515
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
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
Lu, Ren, Keppler, Hans (1997) Water solubility in pyrope to 100 kbar. Contributions to Mineralogy and Petrology, 129 (1) 35-42 doi:10.1007/s004100050321
Guidotti, C. V. (1973) Compositional variation of muscovite as a function of metamorphic grade and assemblage in metapelites from N.W. Maine. Contributions to Mineralogy and Petrology, 42 (1) 33-42 doi:10.1007/bf00521645
Johnston, A. Dana, Wyllie, Peter J. (1988) Constraints on the origin of Archean trondhjemites based on phase relationships of N�k gneiss with H2O at 15 kbar. Contributions to Mineralogy and Petrology, 100 (1) 35-46 doi:10.1007/bf00399438
Storre, Bernhard (1972) Dry melting of muscovite+quartz in the range P s=7 kb to P s=20 kb. Contributions to Mineralogy and Petrology, 37 (1) 87-89 doi:10.1007/bf00377309
Huang, W. L., Wyllie, P. J. (1974) Melting relations of muscovite with quartz and sanidine in the K2O-Al2O3-SiO2-H2O system to 30 kilobars and an outline of paragonite melting relations. American Journal of Science, 274 (4) 378-395 doi:10.2475/ajs.274.4.378
Huang, W. L., Robertson, J. K., Wyllie, P. J. (1973) Melting relations of muscovite to 30 kilobars in the system KAlSi 3 O 8 -Al 2 O 3 -H 2 O. American Journal of Science, 273 (5) 415-427 doi:10.2475/ajs.273.5.415
 
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