Zircon (U‐Th)/He thermochronology of Neoproterozoic strata from the Mackenzie Mountains, Canada: Implications for the Phanerozoic exhumation and deformation history of the northern Canadian Cordillera. Issue 3 (16th March 2016)

• Record Type: Journal Article
• Authors: Powell, Jeremy; Schneider, David; Stockli, Daniel; Fallas, Karen
• Is Part Of: Tectonics. Volume 35:Issue 3(2016)
• Page Start: 663
• Page End: 689
• Publication Date: 2016-03-16
• Subjects: zircon (U‐Th)/He -- thermochronology -- Mackenzie Mountains -- Cordillera; Geology, Structural -- Periodicals; 551.8
• DOI: 10.1002/2015TC003989
• Languages: English
• ISSNs: 0278-7407

Abstract

Abstract: Sedimentary strata of the Neoproterozoic Mackenzie Mountains Supergroup (MMSG) and Windermere Supergroup (WSG) occupy the cores of anticlines in the Mackenzie Mountains of the Canadian Cordilleran Foreland Belt. Stratigraphic and structural evidence suggest that these rocks have undergone several episodes of burial and unroofing relatively intact. We report single‐grain detrital muscovite 40 Ar/ 39 Ar and zircon (U‐Th)/He (ZHe) data from a suite of samples across the fold‐thrust belt and the Neoproterozoic stratigraphic record. The strata have not reached high enough temperatures to reset the muscovite 40 Ar/ 39 Ar system, and instead our detrital muscovite data refine Tonian‐Cryogenian depositional ages. Single‐crystal ZHe dates range from 432 ± 35 to 46 ± 4 Ma, indicating that MMSG and WSG strata have not been heated sufficiently to fully reset the ZHe system. These factors make the Neoproterozoic strata an attractive natural laboratory to test the utility of the zircon radiation damage and annealing model on the quantification of thermal histories from detrital zircon populations that have accumulated radiation damage over long geologic timescales. Thermal modeling reveals that (1) a substantial sedimentary package was deposited following the Devonian and removed during Permo‐Triassic cooling, and (2) the Cordilleran deformation front propagated through the study area from the Albian to the Paleocene, with a moderate increase in cooling rates between 75–67 Ma in the southwest and 60–55 Ma at the deformation front. Ultimately, relationships between radiation damage and helium diffusion kinetics in zircon explain substantial ZHe date dispersion and elucidate the temperature‐time history of the northern Canadian Cordillera. Key Points: Application of ZRDAAM to partially reset ZHe data sets with protracted cooling histories ZHe intrasample date‐eU variance resolves Phanerozoic T‐t history of northern Canadian Cordillera ZHe data illustrate Albian‐Paleocene fold‐thrust belt propagation of Mackenzie Mountains