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Longhi, John, Boudreau, Alan E. (1980) The orthoenstatite liquidus field in the system forsterite-diopside-silica at one atmosphere. American Mineralogist, 65 (5-6) 563-573

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Reference TypeJournal (article/letter/editorial)
TitleThe orthoenstatite liquidus field in the system forsterite-diopside-silica at one atmosphere
JournalAmerican Mineralogist
AuthorsLonghi, JohnAuthor
Boudreau, Alan E.Author
Year1980Volume65
Issue5-6
PublisherMineralogical Society of America
Download URLhttp://www.minsocam.org/ammin/AM65/AM65_563.pdf+
Mindat Ref. ID527441Long-form Identifiermindat:1:5:527441:7
GUID0
Full ReferenceLonghi, John, Boudreau, Alan E. (1980) The orthoenstatite liquidus field in the system forsterite-diopside-silica at one atmosphere. American Mineralogist, 65 (5-6) 563-573
Plain TextLonghi, John, Boudreau, Alan E. (1980) The orthoenstatite liquidus field in the system forsterite-diopside-silica at one atmosphere. American Mineralogist, 65 (5-6) 563-573
In(1980) American Mineralogist Vol. 65 (5-6) Mineralogical Society of America

See Also

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Kushiro, Ikuo (1972) Determination of liquidus relations in synthetic silicate systems with electron probe analysis: The system forsterite-diopside-silica at 1 atmosphere. American Mineralogist, 57 (7-8) 1260-1271
Longhi, John (1991) Comparative liquidus equilibria of hypersthene-normative basalts at low pressure. American Mineralogist, 76 (5-6) 785-800
Nafziger, Ralph H. (1970) The join diopside-iron oxide-silica and its relation to the join diopside-forsterite-iron oxide-silica. American Mineralogist, 55 (11-12) 2042-2052
Dasgupta, S., Gupta, A. K. (2012) THE FORSTERITE-DIOPSIDE-SILICA SYSTEM AT 7 GPA AND ITS SIGNIFICANCE IN THE MELTING BEHAVIOR OF THE MANTLE. The Canadian Mineralogist, 50 (5) 1243-1253 doi:10.3749/canmin.50.5.1243
Kushiro, I. (1969) The system forsterite-diopside-silica with and without water at high pressures. American Journal of Science: 267: 269-294.
Pan, Vivian, Longhi, John (1990) The system Mg2SiO4-Ca2SiO4-CaAl2O4-NaAlSiO4-SiO2: one atmosphere liquidus equilibria of analogs of alkaline mafic lavas. Contributions to Mineralogy and Petrology, 105 (5) 569-584 doi:10.1007/bf00302496
Edgar, A. D. (1964) Phase equilibrium relations in the system CaMgSi2O6(diopside) - NaAlSiO4(nepheline) - NaAlSi3O8(albite) - H2O at 1,000 kg/cm2 water vapor pressure. American Mineralogist, 49 (5-6) 573-585
Sugawara, TORU, Akaogi, Masaki (2003) Heats of mixing of silicate liquid in the systems diopside-anorthite-akermanite, diopside-anorthite-forsterite, and diopside-silica. American Mineralogist, 88 (7) 1020-1024 doi:10.2138/am-2003-0710
Warner, Richard D., Luth, and William C. (1974) The diopside-orthoenstatite two-phase region in the system CaMgSi2O6-Mg2Si2O6. American Mineralogist, 59 (1-2) 98-109
Liu, Teh-ching, Presnall, Dean C. (1989) Diopside-tridymite liquidus boundary line in the system Mg2SiO4-CaMgSi2O6-SiO2 at atmospheric pressure. American Mineralogist, 74 (9-10) 1032-1037
Gupta, A. K., Green, D. H., Taylor, W. R. (1987) The liquidus surface of the system forsterite-nepheline-silica at 28 kb. American Journal of Science, 287 (6) 560-565 doi:10.2475/ajs.287.6.560
 
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