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WUNDER, B., SCHREYER, W. (1992) Metastability of the 10-  Phase in the System MgO-SiO2-H2O (MSH) What about Hydrous MSH Phases in Subduction Zones?. Journal of Petrology, 33 (4) 877-889 doi:10.1093/petrology/33.4.877

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Reference TypeJournal (article/letter/editorial)
TitleMetastability of the 10-  Phase in the System MgO-SiO2-H2O (MSH). What about Hydrous MSH Phases in Subduction Zones?
JournalJournal of Petrology
AuthorsWUNDER, B.Author
SCHREYER, W.Author
Year1992 (August 1)Volume33
Issue4
PublisherOxford University Press (OUP)
DOIdoi:10.1093/petrology/33.4.877Search in ResearchGate
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Mindat Ref. ID179302Long-form Identifiermindat:1:5:179302:8
GUID0
Full ReferenceWUNDER, B., SCHREYER, W. (1992) Metastability of the 10-  Phase in the System MgO-SiO2-H2O (MSH) What about Hydrous MSH Phases in Subduction Zones?. Journal of Petrology, 33 (4) 877-889 doi:10.1093/petrology/33.4.877
Plain TextWUNDER, B., SCHREYER, W. (1992) Metastability of the 10-  Phase in the System MgO-SiO2-H2O (MSH) What about Hydrous MSH Phases in Subduction Zones?. Journal of Petrology, 33 (4) 877-889 doi:10.1093/petrology/33.4.877
In(1992, August) Journal of Petrology Vol. 33 (4) Oxford University Press (OUP)

See Also

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Wunder, Bernd, Schreyer, Werner (1997) Antigorite: High-pressure stability in the system MgO-SiO2-H2O (MSH) Lithos, 41 (1) 213-227 doi:10.1016/s0024-4937(97)82013-0
Wunder, Bernd (1998) quilibrium experiments in the system MgO-SiO2-H2O (MSH): stability fields of clinohumite-OH [Mg9Si4O16(OH)2], chondrodite-OH [Mg5Si2O8(OH)2], and phase A [Mg7Si2O8(OH)2]. Contributions to Mineralogy and Petrology, 132 (2) 111-120 doi:10.1007/s004100050410
FOCKENBERG, T., SCHREYER, W. (1994) Stability of Yoderite in the Absence and in the Presence of Quartz: an Experimental Study in the System MgO-Al2O3-Fe2O3-SiO2-H2O. Journal of Petrology, 35 (5) 1341-1375 doi:10.1093/petrology/35.5.1341
Schreyer, W., Maresch, W.V., Baller, T. (1991) A new hydrous, high-pressure phase with a pumpellyite structure in the system MgO–Al2O3–SiO2–H2O. In Progress in Metamorphic and Magmatic Petrology. Cambridge University Press. p.47-64. doi:10.1017/cbo9780511564444.005
Schreyer, W., Seifert, F. (1967) Metastability of an osumilite end member in the system K2O-MgO-Al2O3-SiO2-H2O and its possible bearing on the rarity of natural osumilites. Contributions to Mineralogy and Petrology, 14 (4) 343-358 doi:10.1007/bf00373812
(2022) Correction to: Melting Phase Equilibria from 4 to 7 GPa in the System CaO-MgO-Al2O3-SiO2-CO2, the Persistence of the ``Ledge'' in Carbonated Basalt with Excess Silica, and the Most Likely Limits on the Depths of Termination of Carbon Cycle at Subduction Zones. Journal of Petrology, 63 (10) doi:10.1093/petrology/egac104
Fransolet, A. -M., Schreyer, W. (1984) Sudoite, di/trioctahedral chlorite: A stable low-temperature phase in the system MgO-Al2O3-SiO2-H2O. Contributions to Mineralogy and Petrology, 86 (4) 409-417 doi:10.1007/bf01187144
Pawley, A. R., Redfern, Simon A. T., Wood, Bernard J. (1995) Thermal expansivities and compressibilities of hydrous phases in the system MgO-SiO2-H2O: talc, phase A and 10-Å phase. Contributions to Mineralogy and Petrology, 122 (3) 301-307 doi:10.1007/s004100050129
WEI, C. (2004) Calculated Phase Relations in High-Pressure Metapelites in the System NKFMASH (Na2O-K2O-FeO-MgO-Al2O3-SiO2-H2O) Journal of Petrology, 45 (1) 183-202 doi:10.1093/petrology/egg085
YANG, JIAN-JUN, POWELL, ROGER (2006) Calculated Phase Relations in the System Na2O–CaO–K2O–FeO–MgO–Al2O3–SiO2–H2O with Applications to UHP Eclogites and Whiteschists. Journal of Petrology, 47 (10) 2047-2071 doi:10.1093/petrology/egl036
Warding, G., Schreyer, W. (1978) Synthesis and crystal chemistry of kornerupine in the system MgO-Al2O3-SiO2-B2O3-H2O. Contributions to Mineralogy and Petrology, 67 (3) 247-259 doi:10.1007/bf00381452
 
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