Magma mixing and the generation of isotopically juvenile silicic magma at Yellowstone caldera inferred from coupling 238U-230Th ages with trace elements and Hf and O isotopes in zircon and Pb isotopes in sanidine

Mark E. Stelten, Kari M. Cooper, Jorge A. Vazquez, Mary Reid, Gry H. Barfod, Josh Wimpenny, Qing zhu Yin

Research output: Contribution to journalArticle

29 Citations (Scopus)

Abstract

The nature of compositional heterogeneity within large silicic magma bodies has important implications for how silicic reservoirs are assembled and evolve through time. We examine compositional heterogeneity in the youngest (~170 to 70 ka) post-caldera volcanism at Yellowstone caldera, the Central Plateau Member (CPM) rhyolites, as a case study. We compare 238U-230Th age, trace-element, and Hf isotopic data from zircons, and major-element, Ba, and Pb isotopic data from sanidines hosted in two CPM rhyolites (Hayden Valley and Solfatara Plateau flows) and one extracaldera rhyolite (Gibbon River flow), all of which erupted near the caldera margin ca. 100 ka. The Hayden Valley flow hosts two zircon populations and one sanidine population that are consistent with residence in the CPM reservoir. The Gibbon River flow hosts one zircon population that is compositionally distinct from Hayden Valley flow zircons. The Solfatara Plateau flow contains multiple sanidine populations and all three zircon populations found in the Hayden Valley and Gibbon River flows, demonstrating that the Solfatara Plateau flow formed by mixing extracaldera magma with the margin of the CPM reservoir. This process highlights the dynamic nature of magmatic interactions at the margins of large silicic reservoirs. More generally, Hf isotopic data from the CPM zircons provide the first direct evidence for isotopically juvenile magmas contributing mass to the youngest post-caldera magmatic system and demonstrate that the sources contributing magma to the CPM reservoir were heterogeneous in 176Hf/177Hf at ca. 100 ka. Thus, the limited compositional variability of CPM glasses reflects homogenization occurring within the CPM reservoir, not a homogeneous source.

Original languageEnglish (US)
Pages (from-to)587-613
Number of pages27
JournalContributions to Mineralogy and Petrology
Volume166
Issue number2
DOIs
StatePublished - Aug 2013

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sanidine
calderas
Trace Elements
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trace elements
Isotopes
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plateaus
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plateau
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Rivers
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river flow
rivers
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Keywords

  • U-Th
  • Hf isotope
  • Mixing
  • Sanidine
  • Yellowstone
  • Zircon

ASJC Scopus subject areas

  • Geochemistry and Petrology
  • Geophysics

Cite this

Magma mixing and the generation of isotopically juvenile silicic magma at Yellowstone caldera inferred from coupling 238U-230Th ages with trace elements and Hf and O isotopes in zircon and Pb isotopes in sanidine. / Stelten, Mark E.; Cooper, Kari M.; Vazquez, Jorge A.; Reid, Mary; Barfod, Gry H.; Wimpenny, Josh; Yin, Qing zhu.

In: Contributions to Mineralogy and Petrology, Vol. 166, No. 2, 08.2013, p. 587-613.

Research output: Contribution to journalArticle

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AU - Stelten, Mark E.

AU - Cooper, Kari M.

AU - Vazquez, Jorge A.

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AU - Yin, Qing zhu

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