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Compositional gradients in large reservoirs of silicic magma as evidenced by ignimbrites versus Taylor Creek Rhyolite lava domes

The Taylor Creek Rhyolite of southwest New Mexico consists of 20 lava domes and flows that were emplaced during a period a few thousand years or less in late Oligocene time. Chemical variations within twenty nearly coeval silicic lava domes and flows are reported.

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Published in:	Contributions to mineralogy and petrology 1992-04, Vol.110 (2-3), p.192-210
Main Authors:	DUFFIELD, Wendell A, RUIZ, Joaquin
Format:	Article
Language:	English
Subjects:	Creeks Crystalline rocks Earth sciences Earth, ocean, space Exact sciences and technology Geochemistry Geology Igneous and metamorphic rocks petrology, volcanic processes, magmas Lava Lava domes Mineralogy Oligocene Petrology Soil and rock geochemistry
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description	The Taylor Creek Rhyolite of southwest New Mexico consists of 20 lava domes and flows that were emplaced during a period a few thousand years or less in late Oligocene time. Chemical variations within twenty nearly coeval silicic lava domes and flows are reported.
doi_str_mv	10.1007/BF00310738
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subjects	Creeks Crystalline rocks Earth sciences Earth, ocean, space Exact sciences and technology Geochemistry Geology Igneous and metamorphic rocks petrology, volcanic processes, magmas Lava Lava domes Mineralogy Oligocene Petrology Soil and rock geochemistry
title	Compositional gradients in large reservoirs of silicic magma as evidenced by ignimbrites versus Taylor Creek Rhyolite lava domes
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