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Duffield, Wendell A., Ruiz, Joaquin (1992) Compositional gradients in large reservoirs of silicic magma as evidenced by ignimbrites versus Taylor Creek Rhyolite lava domes. Contributions to Mineralogy and Petrology, 110 (2) 192-210 doi:10.1007/bf00310738

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Reference TypeJournal (article/letter/editorial)
TitleCompositional gradients in large reservoirs of silicic magma as evidenced by ignimbrites versus Taylor Creek Rhyolite lava domes
JournalContributions to Mineralogy and Petrology
AuthorsDuffield, Wendell A.Author
Ruiz, JoaquinAuthor
Year1992 (April)Volume110
Issue2
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/bf00310738Search in ResearchGate
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Mindat Ref. ID76753Long-form Identifiermindat:1:5:76753:4
GUID0
Full ReferenceDuffield, Wendell A., Ruiz, Joaquin (1992) Compositional gradients in large reservoirs of silicic magma as evidenced by ignimbrites versus Taylor Creek Rhyolite lava domes. Contributions to Mineralogy and Petrology, 110 (2) 192-210 doi:10.1007/bf00310738
Plain TextDuffield, Wendell A., Ruiz, Joaquin (1992) Compositional gradients in large reservoirs of silicic magma as evidenced by ignimbrites versus Taylor Creek Rhyolite lava domes. Contributions to Mineralogy and Petrology, 110 (2) 192-210 doi:10.1007/bf00310738
In(1992, April) Contributions to Mineralogy and Petrology Vol. 110 (2) Springer Science and Business Media LLC

See Also

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Duffield, Wendell A., Ruiz, Joaquin (1992) Evidence for the reversal of gradients in the uppermost parts of silicic magma reservoirs. Geology, 20 (12) 1115 doi:10.1130/0091-7613(1992)020<1115:eftrog>2.3.co;2
Duffield, Wendell A, Dalrymple, G Brent (1990) The Taylor Creek Rhyolite of New Mexico: a rapidly emplaced field of lava domes and flows. Bulletin of Volcanology, 52 (6). 475-487 doi:10.1007/bf00268927
Coulon, C., Dostal, J., Dupuy, C. (1978) Petrology and geochemistry of the ignimbrites and associated lava domes from N.W. Sardinia. Contributions to Mineralogy and Petrology, 68 (1) 89-98 doi:10.1007/bf00375450
Knesel, K. M., Davidson, J. P., Duffield, W. A. (1999) Evolution of Silicic Magma through Assimilation and Subsequent Recharge: Evidence from Sr Isotopes in Sanidine Phenocrysts, Taylor Creek Rhyolite, NM. Journal of Petrology, 40 (5) 773-786 doi:10.1093/petroj/40.5.773
Duffield, Wendell A., Bray, Edward A. Du (1990) Temperature, size, and depth of the magma reservoir for the Taylor Creek Rhyolite, New Mexico. American Mineralogist, 75 (9-10) 1059-1070
Duffield, Wendell A, Ruiz, Joaquin (1998) A model that helps explain Sr-isotope disequilibrium between feldspar phenocrysts and melt in large-volume silicic magma systems. Journal of Volcanology and Geothermal Research, 87 (1) 7-13 doi:10.1016/s0377-0273(98)00071-7
Webster, James D., Duffield, Wendell A. (1994) Extreme halogen abundances in tin-rich magma of the Taylor Creek Rhyolite, New Mexico. Economic Geology, 89 (4) 840-850 doi:10.2113/gsecongeo.89.4.840
Duffield, W.A., Ruiz, Joaquin (1994) A Model to help explain Sr-isotope disequilibrium between feldspar phenocrysts and melt in large-volume silicic magma systems. Open-File Report Vol. 1994 (94-423) US Geological Survey doi:10.3133/ofr94423
Neave, David A. (2020) Chemical variability in peralkaline magmas and magma reservoirs: insights from the Khaggiar lava flow, Pantelleria, Italy. Contributions to Mineralogy and Petrology, 175 (4). doi:10.1007/s00410-020-01678-0
Webster, James D., Duffield, Wendell A. (1991) Volatiles and lithophile elements in Taylor Creek Rhyolite: Constraints from glass inclusion analysis. American Mineralogist, 76 (9-10) 1628-1645
Duffield, Wendell A., Reed, Bruce L., Richter, Donald H. (1990) Origin of rhyolite-hosted tin mineralization; evidence from the Taylor Creek Rhyolite, New Mexico. Economic Geology, 85 (2) 392-398 doi:10.2113/gsecongeo.85.2.392
 
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