U-Th-Pb Geochronology of the Coast Mountains Batholith in North-Coastal British Columbia: Constraints on Age and Tectonic Evolution
U-Th-Pb geochronology of the Coast Mountains batholith in north-coastal British Columbia: Constraints on age and tectonic evolution G. Gehrels1,†, M. Rusmore2, G. Woodsworth3, M. Crawford4, C. Andronicos5, L. Hollister6, J. Patchett1, M. Ducea1, R. Butler7, K. Klepeis8, C. Davidson9, R. Friedman10, J. Haggart3, B. Mahoney11, W. Crawford4, D. Pearson1, and J. Girardi1 1Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA 2Department of Geology, Occidental College, Los Angeles, California 90041, USA 3Geological Survey of Canada, Vancouver, British Columbia V6B-5J3, Canada 4Department of Geology, Bryn Mawr College, Bryn Mawr, Pennsylvania 19010, USA 5Department of Earth and Atmospheric Sciences, Cornell University, Ithaca, New York 14853, USA 6Department of Geosciences, Princeton University, Princeton, New Jersey 08544, USA 7Department of Chemistry and Physics, University of Portland, Portland, Oregon 97203, USA 8Department of Geology, University of Vermont, Burlington, Vermont 05405, USA 9Department of Geology, Carleton College, Northfi eld, Minnesota 55057, USA 10Department of Earth and Ocean Sciences, University of British Columbia, Vancouver, British Columbia V6T 1Z4, Canada 11Department of Geology, University of Wisconsin, Eau Claire, Wisconsin 54702, USA ABSTRACT (5) U-Pb ages of titanite record rapid into southwestern Yukon (Fig. 1). The width of cooling of axial portions of the batholith at the batholith ranges from ~50 to ~150 km. Previously published and new U-Pb geo- ca. 55–48 Ma in response to east-side-down The Coast Mountains batholith provides an chronologic analyses provide 313 zircon and motion on regional extensional structures. important laboratory for studying processes 59 titanite ages that constrain the igneous (6) The magmatic history of this portion of of batholith formation and continental margin and cooling history of the Coast Mountains the Coast Mountains batholith is consistent evolution because (1) it is one of the largest batholith in north-coastal British Columbia.
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