Vote for your favorite mineral in #MinCup25! - Silver vs. Baryte
Are you ready for beautiful utility as sparkling silver competes against hefty baryte?
Log InRegister
Quick Links : The Mindat ManualThe Rock H. Currier Digital LibraryMindat Newsletter [Free Download]
Home PageAbout MindatThe Mindat ManualHistory of MindatCopyright StatusWho We AreContact UsAdvertise on Mindat
Donate to MindatCorporate SponsorshipSponsor a PageSponsored PagesMindat AdvertisersAdvertise on Mindat
Learning CenterWhat is a mineral?The most common minerals on earthInformation for EducatorsMindat ArticlesThe ElementsThe Rock H. Currier Digital LibraryGeologic Time
Minerals by PropertiesMinerals by ChemistryAdvanced Locality SearchRandom MineralRandom LocalitySearch by minIDLocalities Near MeSearch ArticlesSearch GlossaryMore Search Options
Search For:
Mineral Name:
Locality Name:
Keyword(s):
 
The Mindat ManualAdd a New PhotoRate PhotosLocality Edit ReportCoordinate Completion ReportAdd Glossary Item
Mining CompaniesStatisticsUsersMineral MuseumsClubs & OrganizationsMineral Shows & EventsThe Mindat DirectoryDevice SettingsThe Mineral Quiz
Photo SearchPhoto GalleriesSearch by ColorNew Photos TodayNew Photos YesterdayMembers' Photo GalleriesPast Photo of the Day GalleryPhotography

Spear, Frank S. (1988) The Gibbs method and Duhem's theorem: The quantitative relationships among P, T, chemical potential, phase composition and reaction progress in igneous and metamorphic systems. Contributions to Mineralogy and Petrology, 99 (2) 249-256 doi:10.1007/bf00371465

Advanced
   -   Only viewable:
Reference TypeJournal (article/letter/editorial)
TitleThe Gibbs method and Duhem's theorem: The quantitative relationships among P, T, chemical potential, phase composition and reaction progress in igneous and metamorphic systems
JournalContributions to Mineralogy and Petrology
AuthorsSpear, Frank S.Author
Year1988 (June)Volume99
Issue2
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/bf00371465Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID76214Long-form Identifiermindat:1:5:76214:0
GUID0
Full ReferenceSpear, Frank S. (1988) The Gibbs method and Duhem's theorem: The quantitative relationships among P, T, chemical potential, phase composition and reaction progress in igneous and metamorphic systems. Contributions to Mineralogy and Petrology, 99 (2) 249-256 doi:10.1007/bf00371465
Plain TextSpear, Frank S. (1988) The Gibbs method and Duhem's theorem: The quantitative relationships among P, T, chemical potential, phase composition and reaction progress in igneous and metamorphic systems. Contributions to Mineralogy and Petrology, 99 (2) 249-256 doi:10.1007/bf00371465
In(1988, June) Contributions to Mineralogy and Petrology Vol. 99 (2) Springer Science and Business Media LLC

See Also

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

Spear, Frank S. (1988) Metamorphic fractional crystallization and internal metasomatism by diffusional homogenization of zoned garnets. Contributions to Mineralogy and Petrology, 99 (4) 507-517 doi:10.1007/bf00371941
Spear, Frank S. (2024) A grain boundary model of metamorphic reaction. Contributions to Mineralogy and Petrology, 179 (4) doi:10.1007/s00410-024-02100-9
Spear, Frank S., Selverstone, Jane (1983) Quantitative P-T paths from zoned minerals: Theory and tectonic applications. Contributions to Mineralogy and Petrology, 83 (3) 348-357 doi:10.1007/bf00371203
Spear, Frank S. (1988) Thermodynamic projection and extrapolation of high-variance mineral assemblages. Contributions to Mineralogy and Petrology, 98 (3) 346-351 doi:10.1007/bf00375184
Paria, P., Bhattacharya, A., Sen, S. K. (1988) The reaction garnet+clinopyroxene+quartz =2 orthopyroxene+anorthite: A potential geobarometer for granulites. Contributions to Mineralogy and Petrology, 99 (1) 126-133 doi:10.1007/bf00399372
Spear, Frank S., Kohn, Matthew J., Cheney, John T. (1999) Pβ€Š - T paths from anatectic pelites. Contributions to Mineralogy and Petrology, 134 (1) 17-32 doi:10.1007/s004100050466
Florence, Frank P., Spear, Frank S. (1991) Effects of diffusional modification of garnet growth zoning on P-T path calculations. Contributions to Mineralogy and Petrology, 107 (4) 487-500 doi:10.1007/bf00310683
Kohn, Matthew J. (1993) Modeling of prograde mineral ?18O changes in metamorphic systems. Contributions to Mineralogy and Petrology, 113 (2) 249-261 doi:10.1007/bf00283232
Spear, Frank S. (2025) A grain boundary model of garnet growth. Contributions to Mineralogy and Petrology, 180 (2). doi:10.1007/s00410-025-02201-z
Spear, Frank S., Cheney, John T. (1989) A petrogenetic grid for pelitic schists in the system SiO2-Al2O3-FeO-MgO-K2O-H2O. Contributions to Mineralogy and Petrology, 101 (2) 149-164 doi:10.1007/bf00375302
Spear, Frank S. (2025) A grain boundary model of textural evolution of a garnet replacement reaction. Contributions to Mineralogy and Petrology, 180 (8). doi:10.1007/s00410-025-02242-4
 
and/or  
Mindat.org is an outreach project of the Hudson Institute of Mineralogy, a 501(c)(3) not-for-profit organization.
Copyright © mindat.org and the Hudson Institute of Mineralogy 1993-2025, except where stated. Most political location boundaries are Β© OpenStreetMap contributors. Mindat.org relies on the contributions of thousands of members and supporters. Founded in 2000 by Jolyon Ralph.
To cite: Ralph, J., Von Bargen, D., Martynov, P., Zhang, J., Que, X., Prabhu, A., Morrison, S. M., Li, W., Chen, W., & Ma, X. (2025). Mindat.org: The open access mineralogy database to accelerate data-intensive geoscience research. American Mineralogist, 110(6), 833–844. doi:10.2138/am-2024-9486.
Privacy Policy - Terms & Conditions - Contact Us / DMCA issues - Report a bug/vulnerability Current server date and time: September 5, 2025 08:20:48
Go to top of page