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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

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Reference TypeJournal (article/letter/editorial)
TitleThermal expansivities and compressibilities of hydrous phases in the system MgO-SiO2-H2O: talc, phase A and 10-Å phase
JournalContributions to Mineralogy and Petrology
AuthorsPawley, A. R.Author
Redfern, Simon A. T.Author
Wood, Bernard J.Author
Pawley, A. R.Author
Redfern, Simon A. T.Author
Wood, Bernard J.Author
Year1995 (December 11)Volume122
Page(s)301-307Issue3
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s004100050129Search in ResearchGate
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Mindat Ref. ID77335Long-form Identifiermindat:1:5:77335:9
GUID0
Full ReferencePawley, 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
Plain TextPawley, 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
In(1995, December) Contributions to Mineralogy and Petrology Vol. 122 (3) Springer Science and Business Media LLC

Mineral Pages

MineralCitation Details
10 Å Phase
Phase A
Talc

See Also

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

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
Howe, Harriet, Pawley, Alison R. (2019) The effect of solid solution on the stability of talc and 10-Å phase. Contributions to Mineralogy and Petrology, 174 (10) doi:10.1007/s00410-019-1616-0
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
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
Pawley, A. R., Wood, Bernard J. (1996) The low-pressure stability of phase A, Mg 7 Si 2 O 8 (OH) 6. Contributions to Mineralogy and Petrology, 124 (1) 90-97 doi:10.1007/s004100050176
Pawley, Alison R., Chinnery, Nicholas J., Clark, Simon M., Walter, Michael J. (2011) Experimental study of the dehydration of 10-Å phase, with implications for its H2O content and stability in subducted lithosphere. Contributions to Mineralogy and Petrology, 162 (6) 1279-1289 doi:10.1007/s00410-011-0653-0
Wei, Chunjing; Powell, Roger (2003) Phase relations in high-pressure metapelites in the system KFMASH (K2O-FeO-MgO-Al2O3-SiO2-H2O) with application to natural rocks. Contributions to Mineralogy and Petrology, 145 (3). 301-315 doi:10.1007/s00410-003-0454-1
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
Sekine, Toshimori, Wyllie, Peter J. (1982) Phase relationships in the system KAlSiO4-Mg2SiO4-SiO2-H2O as a model for hybridization between hydrous siliceous melts and peridotite. Contributions to Mineralogy and Petrology, 79 (4) 368-374 doi:10.1007/bf01132066
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
Trommsdorff, Volkmar, Connolly, James A. D. (1990) Constraints on phase diagram topology for the system CaO?MgO?SiO2?CO2?H2O. Contributions to Mineralogy and Petrology, 104 (1) 1-7 doi:10.1007/bf00310641
 
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