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Holness, Marian B. (1995) The effect of feldspar on quartz-H2O−CO2 dihedral angles at 4 kbar, with consequences for the behaviour of aqueous fluids in migmatites. Contributions to Mineralogy and Petrology, 118 (4) 356-364 doi:10.1007/s004100050020

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Reference TypeJournal (article/letter/editorial)
TitleThe effect of feldspar on quartz-H2O−CO2 dihedral angles at 4 kbar, with consequences for the behaviour of aqueous fluids in migmatites
JournalContributions to Mineralogy and Petrology
AuthorsHolness, Marian B.Author
Year1995 (January)Volume118
Issue4
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s004100050020Search in ResearchGate
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Mindat Ref. ID77133Long-form Identifiermindat:1:5:77133:3
GUID0
Full ReferenceHolness, Marian B. (1995) The effect of feldspar on quartz-H2O−CO2 dihedral angles at 4 kbar, with consequences for the behaviour of aqueous fluids in migmatites. Contributions to Mineralogy and Petrology, 118 (4) 356-364 doi:10.1007/s004100050020
Plain TextHolness, Marian B. (1995) The effect of feldspar on quartz-H2O−CO2 dihedral angles at 4 kbar, with consequences for the behaviour of aqueous fluids in migmatites. Contributions to Mineralogy and Petrology, 118 (4) 356-364 doi:10.1007/s004100050020
In(1995, January) Contributions to Mineralogy and Petrology Vol. 118 (4) Springer Science and Business Media LLC

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Holness, Marian B., Graham, Colin M. (1991) Equilibrium dihedral angles in the system H2O−CO2−NaCl-calcite, and implications for fluid flow during metamorphism. Contributions to Mineralogy and Petrology, 108 (3) 368-383 doi:10.1007/bf00285944
Holness, M. B., Graham, C. M. (1995) P-T-X effects on equilibrium carbonate-H2O-CO2-NaCl dihedral angles: constraints on carbonate permeability and the role of deformation during fluid infiltration. Contributions to Mineralogy and Petrology, 119 (2) 301-313 doi:10.1007/bf00307289
Holness, Marian B. (1993) Temperature and pressure dependence of quartz-aqueous fluid dihedral angles: the control of adsorbed H2O on the permeability of quartzites. Earth and Planetary Science Letters, 117 (3) 363-377 doi:10.1016/0012-821x(93)90090-v
Holness, Marian B., Bickle, M. J., Graham, Colin M. (1991) On the kinetics of textural equilibration in forsterite marbles. Contributions to Mineralogy and Petrology, 108 (3) 356-367 doi:10.1007/bf00285943
Holness, Marian B. (1992) Equilibrium dihedral angles in the system quartz-CO2H2ONaCl at 800°C and 1–15 kbar: the effects of pressure and fluid composition on the permeability of quartzites. Earth and Planetary Science Letters, 114 (1) 171-184 doi:10.1016/0012-821x(92)90159-s
Holness, Marian B. (2014) The effect of crystallization time on plagioclase grain shape in dolerites. Contributions to Mineralogy and Petrology, 168 (5) doi:10.1007/s00410-014-1076-5
Cruz, Miguel F., Manning, Craig E. (2015) Experimental determination of quartz solubility and melting in the system SiO2–H2O–NaCl at 15–20 kbar and 900–1100 °C: implications for silica polymerization and the formation of supercritical fluids. Contributions to Mineralogy and Petrology, 170 (4) doi:10.1007/s00410-015-1187-7
Williams, T. J., Candela, Philip A., Piccoli, Philip M. (1995) The partitioning of copper between silicate melts and two-phase aqueous fluids: An experimental investigation at 1 kbar, 800° C and 0.5 kbar, 850° C. Contributions to Mineralogy and Petrology, 121 (4) 388-399 doi:10.1007/s004100050104
Holness, M. B., Graham, C. M. (1995) P-T-X effects on equilibrium carbonate-H 2 O-CO 2 -NaCl dihedral angles: constraints on carbonate permeability and the role of deformation during fluid infiltration. Contributions to Mineralogy and Petrology, 119 (2) 301-313 doi:10.1007/s004100050044
Mason, R. A. (1979) The ordering behaviour of albite in aqueous solutions at 1 kbar. Contributions to Mineralogy and Petrology, 68 (3) 269-273 doi:10.1007/bf00371547
Shmulovich, Kirill, Graham, Colin, Yardley, Bruce (2001) Quartz, albite and diopside solubilities in H2O–NaCl and H2O–CO2 fluids at 0.5–0.9 GPa. Contributions to Mineralogy and Petrology, 141 (1) 95-108 doi:10.1007/s004100000224
 
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