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Brunet, Fabrice, Chopin, Christian, Seifert, Friedrich (1998) Phase relations in the MgO–P2O5–H2O system and the stability of phosphoellenbergerite: petrological implications. Contributions to Mineralogy and Petrology, 131 (1) 54-70 doi:10.1007/s004100050378

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Reference TypeJournal (article/letter/editorial)
TitlePhase relations in the MgO–P2O5–H2O system and the stability of phosphoellenbergerite: petrological implications
JournalContributions to Mineralogy and Petrology
AuthorsBrunet, FabriceAuthor
Chopin, ChristianAuthor
Seifert, FriedrichAuthor
Brunet, FabriceAuthor
Chopin, ChristianAuthor
Seifert, FriedrichAuthor
Year1998 (March 30)Volume131
Page(s)54-70Issue1
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s004100050378Search in ResearchGate
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Mindat Ref. ID77620Long-form Identifiermindat:1:5:77620:4
GUID0
Full ReferenceBrunet, Fabrice, Chopin, Christian, Seifert, Friedrich (1998) Phase relations in the MgO–P2O5–H2O system and the stability of phosphoellenbergerite: petrological implications. Contributions to Mineralogy and Petrology, 131 (1) 54-70 doi:10.1007/s004100050378
Plain TextBrunet, Fabrice, Chopin, Christian, Seifert, Friedrich (1998) Phase relations in the MgO–P2O5–H2O system and the stability of phosphoellenbergerite: petrological implications. Contributions to Mineralogy and Petrology, 131 (1) 54-70 doi:10.1007/s004100050378
In(1998, March) Contributions to Mineralogy and Petrology Vol. 131 (1) Springer Science and Business Media LLC

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MineralCitation Details
Phosphoellenbergerite

Mineral Occurrences

LocalityMineral(s)
Dora-Maira coesite-bearing unit, Cuneo Province, Piedmont, Italyⓘ Phosphoellenbergerite

See Also

These are possibly similar items as determined by title/reference text matching only.

Brunet, Fabrice, Chopin, Christian (1995) Bearthite, Ca2Al(PO4)2OH: stability, thermodynamic properties and phase relations. Contributions to Mineralogy and Petrology, 121 (3) 258-266 doi:10.1007/bf02688241
Olesch, Martin, Seifert, Friedrich (1981) The restricted stability of osumilite under hydrous conditions in the system K2O-MgO?Al2O3?SiO2?H2O. Contributions to Mineralogy and Petrology, 76 (3) 362-367 doi:10.1007/bf00375463
Seifert, F., Schreyer, W. (1971) Synthesis and stability of micas in the system K2O-MgO-SiO2-H2O and their relations to phlogopite. Contributions to Mineralogy and Petrology, 30 (3) 196-215 doi:10.1007/bf00455671
Seifert, F. (1973) Stability of the assemblage cordierite—Corundum in the system MgO-Al2O3-SiO2-H2O. Contributions to Mineralogy and Petrology, 41 (2) 171-177 doi:10.1007/bf00375041
Annersten, H., Seifert, F. (1981) Stability of the assemblage orthopyroxene-sillimanite-quartz in the system MgO-FeO-Fe2O3-Al2O3-SiO2-H2O. Contributions to Mineralogy and Petrology, 77 (2) 158-165 doi:10.1007/bf00636519
Trommsdorff, Volkmar, Evans, Bernard W. (1977) Antigorite-ophicarbonates: Phase relations in a portion of the system CaO-MgO-SiO2-H2O-CO2. Contributions to Mineralogy and Petrology, 60 (1) 39-56 doi:10.1007/bf00372850
Jenkins, David M. (1981) Experimental phase relations of hydrous peridotites modelled in the system H2O-CaO-MgO-Al2O3,-SiO2. Contributions to Mineralogy and Petrology, 77 (2) 166-176 doi:10.1007/bf00636520
Christy, Andrew G. (1989) The stability of sapphirine + clinopyroxene: implications for phase relations in the CaO-MgO-Al2O3-SiO2 system under deep-crustal and upper mantle conditions. Contributions to Mineralogy and Petrology, 102 (4) 422-428 doi:10.1007/bf00371085
Pawley, Alison (2000) Stability of clinohumite in the system MgO-SiO2-H2O. Contributions to Mineralogy and Petrology, 138 (3) 284-291 doi:10.1007/s004100050563
Chatterjee, Niranjan D., Johannes, Wilhelm, Leistner, Hans (1984) The system CaO-Al2O3-SiO2-H2O: new phase equilibria data, some calculated phase relations, and their petrological applications. Contributions to Mineralogy and Petrology, 88 (1) 1-13 doi:10.1007/bf00371407
Fockenberg, Thomas (1998) An experimental investigation on the P-T stability of Mg-staurolite in the system MgO-Al2O3-SiO2-H2O. Contributions to Mineralogy and Petrology, 130 (2). 187-198 doi:10.1007/s004100050359
 
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