Abstract
Zircon U–Pb geochronology results indicate that the John Muir Intrusive Suite of the central Sierra Nevada batholith, California, was assembled over a period of at least 12 Ma between 96 and 84 Ma. Bulk mineral thermochronology (U–Pb zircon and titanite, 40Ar/39Ar hornblende and biotite) of rocks from multiple plutons comprising the Muir suite indicates rapid cooling through titanite and hornblende closure following intrusion and subsequent slow cooling through biotite closure. Assembly of intrusive suites in the Sierra Nevada and elsewhere over millions of years favors growth by incremental intrusion. Estimated long-term pluton assembly rates for the John Muir Intrusive Suite are on the order of 0.001 km3 a−1 which is inconsistent with the rapid magma fluxes that are necessary to form large-volume magma chambers capable of producing caldera-forming eruptions. If large shallow crustal magma chambers do not typically develop during assembly of large zoned intrusive suites, it is doubtful that the intrusive suites represent cumulates left behind following caldera-forming eruptions.
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Acknowledgments
This research was supported by National Science Foundation grant EAR-0538129 awarded to Coleman and EAR- 0538094 awarded to John Bartley (University of Utah). Additional funding was provided by Sigma Xi (J. Davis, J. Gracely), the Geological Society of America (J. Davis, M. Stearns), the White Mountain Research Station (J. Davis, J. Gracely, R. Gaschnig), the University of Utah Department of Geology and Geophysics (M. Stearns), and the Martin Fellowship and Charles S. Bartlett funds administered by the University of North Carolina at Chapel Hill (J. Davis, J. Gracely, R. Gaschnig). We would like to especially acknowledge Allen Glazner, John Bartley, Matt Heizler for reviewing this manuscript and providing thoughtful insight pertaining to the issues addressed here. Special thanks to Matt Heizler and Lisa Peters who provided technical support at the New Mexico Geochronology Research Laboratory, New Mexico Bureau of Geology. We thank Jon Blundy, Luca Caricchi, and an anonymous reviewer for thoughtful insights and comments regarding this manuscript. Logistical support from Kings Canyon Nation Park and the National Forest Service is greatly appreciated.
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Davis, J.W., Coleman, D.S., Gracely, J.T. et al. Magma accumulation rates and thermal histories of plutons of the Sierra Nevada batholith, CA. Contrib Mineral Petrol 163, 449–465 (2012). https://doi.org/10.1007/s00410-011-0683-7
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DOI: https://doi.org/10.1007/s00410-011-0683-7