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Geology; August 2000; v. 28; no. 8; p. 719-722; DOI: 10.1130/0091-7613(2000)28<719:FOLRAC>2.0.CO;2
© 2000 Geological Society of America
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Formation of low-{delta}18O rhyolites after caldera collapse at Yellowstone, Wyoming, USA

Ilya N. Bindeman1 and John W. Valley1

1 Department of Geology and Geophysics, University of Wisconsin, 1215 West Dayton Street, Madison, Wisconsin 53706, USA

We present a new model for the genesis of low-{delta}18O rhyolites of the Yellowstone caldera based on analyses of zircons and individual quartz phenocrysts. Low-{delta}18O rhyolites were erupted soon after the massive caldera-forming Lava Creek Tuff eruption (602 ka, ~1000 km3) and contain xenocrysts of quartz and zircon inherited from precaldera rhyolites. These zircons are isotopically zoned and out of equilibrium with their host low-{delta}18O melts and quartz. Diffusion modeling predicts that magmatic disequilibria of oxygen isotopes persists for as much as tens of thousands of years following nearly total remelting of the hydrothermally altered igneous roots of the depressed cauldron, in which the alteration-resistant quartz and zircon initially retained their {delta}18O values. These results link melting to caldera collapse, rule out rapid or catastrophic magma–meteoric water interaction, and indicate wholesale melting rather than assimilation or partial melting.

Key Words: Yellowstone • zircon • oxygen isotopes • caldera • low {delta}18O




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