10 Jurassic to Cenozoic Geology of Southern California, Southwest Arizona, and Sonora: A Session Honoring Gordon Haxel and Carl Jacobson (Posters)
Tuesday, 15 May 2018
8:30 AM - 6:30 PM
Outdoor Tents
RAPID CONSTRUCTION OF THE MIOCENE AZTEC WASH PLUTON (NEVADA) FROM HIGH-PRECISION U-PB ZIRCON GEOCHRONOLOGY
Paper number: 10-10
Program: Symposia Sessions
Time: 8:30 AM – 6:30 PM
Authors
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Terrence J. BlackburnUniversity of California Santa Cruz, Santa Cruz, CA
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Jonathan S. MillerSan Jose State University, San Jose, CA
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Andrew R.C. Kylander-ClarkUniversity of California Santa Barbara, Santa Barbara, CA
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Graham H. EdwardsUniversity of California Santa Cruz, Santa Cruz, CA
Abstract
New high-precision CA-ID-TIMS U-Pb geochronology has been undertaken to better constrain the duration of construction of Aztec Wash pluton. Sampling was conducted on 8 mafic sheets (from the 3 major mafic pulses) from the deepest to shallowest parts of the pluton; mafic sheets were chosen to constrain the timing because the magmas that formed these sheets were initially undersaturated in zircon when intruded, and thus reached saturation late in residual melts and contain little inherited zircon. This is corroborated by CL imaging that shows relatively simple internal zoning and similar intersample trace element geochemistry. Preliminary weighted mean U-Pb dates suggest that the entire Aztec Wash pluton was emplaced over a maximum duration of 60,000 yrs but an age difference the between structurally highest and lowest mafic lobes cannot currently be resolved; more data are needed to better refine the dates of several samples.
Although the construction of the intrusion may have waxed and waned between major mafic pulses, the short emplacement timescale over the entire 5 km exposure depth implies a persistent and dynamic granitic magma body that was thermally maintained by repeated mafic injections. This would also have permitted repeated extensive hybridization between mafic input and granitic magma and mush as observed throughout Aztec Wash pluton.
Geological Society of America Abstracts with Programs. Vol. 50, No. 5
doi: 10.1130/abs/2018RM-314026
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