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London, David, Morgan, George B., Icenhower, Jonathan (2017) Erratum: Stability and Solubility of Pollucite In the Granite System At 200 MPa H2O. The Canadian Mineralogist, 55 (5) 945-946 doi:10.3749/canmin.er00001

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Reference TypeJournal (article/letter/editorial)
TitleErratum: Stability and Solubility of Pollucite In the Granite System At 200 MPa H2O
JournalThe Canadian Mineralogist
AuthorsLondon, DavidAuthor
Morgan, George B.Author
Icenhower, JonathanAuthor
Year2017 (September)Volume55
Issue5
PublisherMineralogical Association of Canada
DOIdoi:10.3749/canmin.er00001Search in ResearchGate
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Mindat Ref. ID65468Long-form Identifiermindat:1:5:65468:3
GUID0
Full ReferenceLondon, David, Morgan, George B., Icenhower, Jonathan (2017) Erratum: Stability and Solubility of Pollucite In the Granite System At 200 MPa H2O. The Canadian Mineralogist, 55 (5) 945-946 doi:10.3749/canmin.er00001
Plain TextLondon, David, Morgan, George B., Icenhower, Jonathan (2017) Erratum: Stability and Solubility of Pollucite In the Granite System At 200 MPa H2O. The Canadian Mineralogist, 55 (5) 945-946 doi:10.3749/canmin.er00001
In(2017, September) The Canadian Mineralogist Vol. 55 (5) Mineralogical Association of Canada

See Also

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

London, D., Morgan, G.B., VI, and Icehower, J. (1998) Stability and solubility of pollucite in granitic system at 200 MPa H2O. Canadian Mineralogist: 36: 497-510.
Icenhower, Jonathan, London, David (1995) An experimental study of element partitioning among biotite, muscovite, and coexisting peraluminous silicic melt at 200 MPa (H2O) American Mineralogist, 80 (11) 1229-1251 doi:10.2138/am-1995-11-1213
London, David, Morgan, George B., Babb, Harold A., Loomis, Jennifer L. (1993) Behavior and effects of phosphorus in the system Na2O−K2O−Al2O3−SiO2−P2O5−H2O at 200 MPa(H2O) Contributions to Mineralogy and Petrology, 113 (4) 450-465 doi:10.1007/bf00698315
London, David, Morgan, George B., Hervig, Richard L. (1989) Vapor-undersaturated experiments with Macusani glass+H2O at 200 MPa, and the internal differentiation of granitic pegmatites. Contributions to Mineralogy and Petrology, 102 (1) 1-17 doi:10.1007/bf01160186
Schneider, Jonathan B., Jenkins, David M. (2020) Stability of sodalite relative to nepheline in NaCl–H2O brines at 750 °C: Implications for hydrothermal formation of sodalite. The Canadian Mineralogist, 58 (1) 3-18 doi:10.3749/canmin.1900031
London, David, Hervig, Richard L., Morgan, George B. (1988) Melt-vapor solubilities and elemental partitioning in peraluminous granite-pegmatite systems: experimental results with Macusani glass at 200 MPa. Contributions to Mineralogy and Petrology, 99 (3) 360-373 doi:10.1007/bf00375368
Acosta-Vigil, Antonio, London, David, Morgan, George B. (2006) Experiments on the kinetics of partial melting of a leucogranite at 200 MPa H2O and 690–800°C: compositional variability of melts during the onset of H2O-saturated crustal anatexis. Contributions to Mineralogy and Petrology, 151 (5) 539-557 doi:10.1007/s00410-006-0081-8
Morgan, George B., London, David (1989) Experimental reactions of amphibolite with boron-bearing aqueous fluids at 200 MPa: implications for tourmaline stability and partial melting in mafic rocks. Contributions to Mineralogy and Petrology, 102 (3) 281-297 doi:10.1007/bf00373721
Morgan, George B., Acosta-Vigil, Antonio, London, David (2008) Diffusive equilibration between hydrous metaluminous-peraluminous haplogranite liquid couples at 200 MPa (H2O) and alkali transport in granitic liquids. Contributions to Mineralogy and Petrology, 155 (2) 257-269 doi:10.1007/s00410-007-0242-4
Morgan VI, George B., London, David (2005) Phosphorus distribution between potassic alkali feldspar and metaluminous haplogranitic liquid at 200 MPa (H2O): the effect of undercooling on crystal–liquid systematics. Contributions to Mineralogy and Petrology, 150 (4) 456-471 doi:10.1007/s00410-005-0034-7
Acosta-Vigil, Antonio, London, David, Morgan VI, George B. (2005) Contrasting interactions of sodium and potassium with H2O in haplogranitic liquids and glasses at 200 MPa from hydration–diffusion experiments. Contributions to Mineralogy and Petrology, 149 (3) 276-287 doi:10.1007/s00410-004-0648-1
 
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