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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

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Reference TypeJournal (article/letter/editorial)
TitleP-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
JournalContributions to Mineralogy and Petrology
AuthorsHolness, M. B.Author
Graham, C. M.Author
Year1995 (March 1)Volume119
Issue2
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s004100050044Search in ResearchGate
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Mindat Ref. ID77184Long-form Identifiermindat:1:5:77184:7
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Full ReferenceHolness, 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
Plain TextHolness, 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
In(1995, March) Contributions to Mineralogy and Petrology Vol. 119 (2) Springer Science and Business Media LLC

See Also

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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., 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., Bickle, M. J., Graham, C. M. (1992) Reply to comments ?On the kinetics of textural equilibrium in forsterite marbles? by M.B. Holness, M.J. Bickle and C.M. Graham. Contributions to Mineralogy and Petrology, 111 (3) 421-422 doi:10.1007/bf00311202
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
Shmulovich, Kirill I., Graham, Colin M. (1999) An experimental study of phase equilibria in the system H 2 O-CO 2 -NaCl at 800 °C and 9 kbar. Contributions to Mineralogy and Petrology, 136 (3) 247-257 doi:10.1007/s004100050536
Ferry, J. M. (1976) P, T, $$f_{{\text{CO}}_{\text{2}} }$$ and $$f_{{\text{H}}_{\text{2}} {\text{O}}}$$ during metamorphism of calcareous sediments in the Waterville-Vassalboro area, south-central Maine. Contributions to Mineralogy and Petrology, 57 (2) 119-143 doi:10.1007/bf00405221
Ferry, John M., Gottschalk, Matthias (2009) The effect of fluid salinity on infiltration-driven contact metamorphism of carbonate rocks. Contributions to Mineralogy and Petrology, 158 (5) 619-636 doi:10.1007/s00410-009-0400-y
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
Lewis, Stephanie, Holness, Marian (1996) Equilibrium halite-H2O dihedral angles: High rock-salt permeability in the shallow crust?. Geology, 24 (5) 431 doi:10.1130/0091-7613(1996)024<0431:ehhoda>2.3.co;2
Shmulovich, Kirill I., Graham, C. M. (1996) Melting of albite and dehydration of brucite in H 2 O-NaCl fluids to 9 kbars and 700-900°C: implications for partial melting and water activities during high pressure metamorphism. Contributions to Mineralogy and Petrology, 124 (3) 370-382 doi:10.1007/s004100050197
 
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