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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

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Reference TypeJournal (article/letter/editorial)
TitleExperimental study of the dehydration of 10-Å phase, with implications for its H2O content and stability in subducted lithosphere
JournalContributions to Mineralogy and Petrology
AuthorsPawley, Alison R.Author
Chinnery, Nicholas J.Author
Clark, Simon M.Author
Walter, Michael J.Author
Year2011 (December)Volume162
Issue6
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s00410-011-0653-0Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID79262Long-form Identifiermindat:1:5:79262:8
GUID0
Full ReferencePawley, 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
Plain TextPawley, 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
In(2011, December) Contributions to Mineralogy and Petrology Vol. 162 (6) Springer Science and Business Media LLC

See Also

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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
Pawley, Alison R. (1994) The pressure and temperature stability limits of lawsonite: implications for H2O recycling in subduction zones. Contributions to Mineralogy and Petrology, 118 (1) 99-108 doi:10.1007/bf00310614
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
Pawley, Alison (2003) Chlorite stability in mantle peridotite: the reaction clinochlore+enstatite=forsterite+pyrope+H2O. Contributions to Mineralogy and Petrology, 144 (4) 449-456 doi:10.1007/s00410-002-0409-y
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
Bromiley, Geoffrey D., Pawley, Alison R. (2002) The high-pressure stability of Mg-sursassite in a model hydrous peridotite: a possible mechanism for the deep subduction of significant volumes of H2O. Contributions to Mineralogy and Petrology, 142 (6) 714-723 doi:10.1007/s00410-001-0318-5
Hermann, Jörg, Troitzsch, Ulrike, Scott, Dean (2016) Experimental subsolidus phase relations in the system CaCO3–CaMg(CO3)2 up to 6.5 GPa and implications for subducted marbles. Contributions to Mineralogy and Petrology, 171 (10) doi:10.1007/s00410-016-1296-y
Cavosie, Aaron J., Valley, John W., Kita, Noriko T., Spicuzza, Michael J., Ushikubo, Takayuki, Wilde, Simon A. (2011) The origin of high δ18O zircons: marbles, megacrysts, and metamorphism. Contributions to Mineralogy and Petrology, 162 (5) 961-974 doi:10.1007/s00410-011-0634-3
Pawley, A.R. (1994) The pressure and temperature stability limits of lawsonite: implications for H2O recycling in subduction zones. Contributions to Mineralogy and Petrology: 118: 99-108.
Norberg, Nicholas, Neusser, Gregor, Wirth, Richard, Harlov, Daniel (2011) Microstructural evolution during experimental albitization of K-rich alkali feldspar. Contributions to Mineralogy and Petrology, 162 (3) 531-546 doi:10.1007/s00410-011-0610-y
Hermann, Jörg (2002) Experimental constraints on phase relations in subducted continental crust. Contributions to Mineralogy and Petrology, 143 (2) 219-235 doi:10.1007/s00410-001-0336-3
 
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