Thermochronology in southeast Alaska and southwest Yukon: Implications for North American Plate response to terrane accretion

Enkelmann, E., Piestrzeniewicz, A., Falkowski, S. , Stübner, K. and Ehlers, T. A. (2017) Thermochronology in southeast Alaska and southwest Yukon: Implications for North American Plate response to terrane accretion. Earth and Planetary Science Letters, 457, pp. 348-358. (doi: 10.1016/j.epsl.2016.10.032)

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Abstract

This study presents the first comprehensive dataset of low-temperature thermochronology from 43 bedrock samples collected north of the active Yakutat–North American plate boundary. Our apatite and zircon (U–Th)/He and fission-track data reveal the cooling history of the inboard Wrangellia Composite Terrane that is dominated by rapid cooling after Late Jurassic to Early Cretaceous arc magmatism followed by very little cooling and exhumation until today. Deformation resulting in rock exhumation due to the collision of the Yakutat microplate is spatially very limited (20–30 km) and is concentrated mainly in the Chugach–Prince William Terrane and rocks near the Border Ranges Fault. Focused exhumation from greater depths of ca. 10 km with very high rates (>5 km/Myr) is localized at the syntaxis region, starting ca. 10 Ma and shifted south through time. The rapid exhumation rates are explained by the development of strong feedbacks between tectonically driven surface uplift and erosion, which started already before glaciation of the area. The shift in the location towards the south is a consequence of continuous readjusting between tectonics and climate, which is changing on local and global scales since the Late Miocene.

Item Type:Articles
Status:Published
Refereed:Yes
Glasgow Author(s) Enlighten ID:Falkowski, Dr Sarah and Ehlers, Professor Todd A.
Authors: Enkelmann, E., Piestrzeniewicz, A., Falkowski, S., Stübner, K., and Ehlers, T. A.
College/School:College of Science and Engineering > School of Geographical and Earth Sciences
Journal Name:Earth and Planetary Science Letters
Publisher:Elsevier
ISSN:0012-821X
ISSN (Online):1385-013X

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