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Dahl, Peter S. (1980) The thermal-compositional dependence of Fe2+-Mg distributions between coexisting garnet and pyroxene: applications to geothermometry. American Mineralogist, 65 (9-10) 852-866

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Reference TypeJournal (article/letter/editorial)
TitleThe thermal-compositional dependence of Fe2+-Mg distributions between coexisting garnet and pyroxene: applications to geothermometry
JournalAmerican Mineralogist
AuthorsDahl, Peter S.Author
Year1980Volume65
Issue9-10
PublisherMineralogical Society of America
Download URLhttp://www.minsocam.org/ammin/AM65/AM65_852.pdf+
Mindat Ref. ID527482Long-form Identifiermindat:1:5:527482:0
GUID0
Full ReferenceDahl, Peter S. (1980) The thermal-compositional dependence of Fe2+-Mg distributions between coexisting garnet and pyroxene: applications to geothermometry. American Mineralogist, 65 (9-10) 852-866
Plain TextDahl, Peter S. (1980) The thermal-compositional dependence of Fe2+-Mg distributions between coexisting garnet and pyroxene: applications to geothermometry. American Mineralogist, 65 (9-10) 852-866
In(1980) American Mineralogist Vol. 65 (9-10) Mineralogical Society of America

See Also

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Bishop, F. C. (1980) The distribution of Fe (super 2+) and Mg between coexisting ilmenite and pyroxene with applications to geothermometry. American Journal of Science, 280 (1) 46-77 doi:10.2475/ajs.280.1.46
Dallmeyer, R. D. (1974) The role of crystal structure in controlling the partitioning of Mg and Fe2+ between coexisting garnet and biotite. American Mineralogist, 59 (1-2) 201-203
Dahl, Peter S. (1979) Comparative geothermometry based on major-element and oxygen isotope distributions in Precambrian metamorphic rocks from southwestern Montana. American Mineralogist, 64 (11-12) 1280-1293
Frost, Daniel J. (2003) Fe2+-Mg partitioning between garnet, magnesiowĂĽstite, and (Mg,Fe)2SiO4 phases of the transition zone. American Mineralogist, 88 (2) 387-397 doi:10.2138/am-2003-2-315
Ravna, Erling Krogh (2000) Distribution of Fe2+ and Mg between coexisting garnet and hornblende in synthetic and natural systems: an empirical calibration of the garnet–hornblende Fe–Mg geothermometer. Lithos, 53 (3) 265-277 doi:10.1016/s0024-4937(00)00029-3
Hackler, Roderick T., Wood, Bernard J. (1989) Experimental determination of Fe and Mg exchange between garnet and olivine and estimation of Fe-Mg mixing properties in garnet. American Mineralogist, 74 (9-10) 994-999
Buddington, A. F. (1950) Composition and genesis of pyroxene and garnet related to Adirondack anorthosite and anorthosite marble contact zones. American Mineralogist, 35 (9-10) 659-670
Podvin, Pascal (1988) Ni-Mg partitioning between synthetic olivines and orthopyroxenes: Application to geothermometry. American Mineralogist, 73 (3-4) 274-280
Maxey, L. R., Vogel, T. A. (1974) Compositional dependence of the coexisting pyroxene iron-magnesium distribution coefficient. Contributions to Mineralogy and Petrology, 43 (4) 295-306 doi:10.1007/bf00373485
Saxena, S. K. (1968) Distribution of elements between coexisting minerals and the nature of solid solution in garnet. American Mineralogist, 53 (5-6) 994-1014
Oka, Yasutami, Matsumoto, Takashi (1974) Study on the compositional dependence of the apparent partition coefficient of iron and magnesium between coexisting garnet and clinopyroxene solid solution. Contributions to Mineralogy and Petrology, 48 (2) 115-121 doi:10.1007/bf00418613
 
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