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            "Department of Geology and Geophysics, University of Wisconsin, 1215 West Dayton Street, Madison, WI 53706, USA"
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    "description": "Zircons from Cretaceous and Tertiary granitic rocks of the Idaho batholith preserve the best record of magmatic oxygen isotope ratios. The coupling of oxygen isotope data from refractory minerals, such as zircon and garnet, with that from less refractory minerals, such as quartz, reveals the complex evolution and alteration history of the Idaho batholith. Values of \u03b418O(Zircon) throughout the batholith are relatively homogeneous at 6.9\u00b10.9\u2030 (1 SD, n=21 rocks), despite variations in age and chemistry. Samples from the Bitterroot lobe have an average \u03b418O(Zircon) of 7.1\u00b10.3\u2030 (n=7 rocks), and samples from the Atlanta lobe have an average \u03b418O(Zircon) of 7.0\u00b11.0\u2030 (n=9 rocks). Four epizonal Tertiary plutons have an average \u03b418O(Zircon) of 7.2\u00b10.2\u2030 (n=4 rocks). These data indicate a similar magmatic source for all granitic rocks of the Idaho batholith except the Tertiary epizonal Casto pluton which has a \u03b418O(Zircon) of 4.0\u00b10.1\u2030 (n=1 rock). The zircon data show that the range of normal magmatic \u03b418O is considerably more restricted than was previously inferred, despite some samples containing two micas and/or garnet, or having a mildly peraluminous character. Quartz is more variable than zircon in \u03b418O. Average \u03b418O(Quartz) for the entire batholith is 10.4\u00b11.1\u2030 (1 SD, n=65 rocks) with a range of 7.7 to 12.4\u2030, excluding the Casto pluton. The spread of quartz values is 2.7\u2030 larger and typically higher than that calculated relative to zircon. Quartz data from the Bitterroot lobe and epizonal Tertiary plutons suggest the alteration of primary \u03b418O during metamorphic events. Quartz data from the Atlanta lobe suggest closed system diffusional exchange during cooling. Igneous garnet \u03b418O values are higher than, and out of equilibrium with, those of coexisting zircon by 0.1\u20130.9\u2030. Assuming an average \u03b418O for unaltered wall-rock metasediments, the incorporation of 10% metasediment into a magma after crystallization of zircon raises the \u03b418O(Magma) by 0.9\u2030, the largest measured \u0394(Garnet-Zircon). These quartz and garnet \u03b418O from the Atlanta and Bitterroot lobes suggest magmatic contamination with a high-\u03b418O rock after the crystallization of zircon, and before that of garnet and quartz.", 
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        "name": "Contributions to Mineralogy and Petrology", 
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        "volumeNumber": "142"
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    "name": "The source, magmatic contamination, and alteration of the Idaho batholith", 
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