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• W2124372616 abstract "Research Article| October 01, 2006 Fault dating in the Canadian Rocky Mountains: Evidence for late Cretaceous and early Eocene orogenic pulses Ben A. van der Pluijm; Ben A. van der Pluijm 1Department of Geological Sciences, University of Michigan, Ann Arbor, Michigan 48109, USA Search for other works by this author on: GSW Google Scholar Peter J. Vrolijk; Peter J. Vrolijk 2ExxonMobil Upstream Research Company, Houston, Texas 77252-2189, USA Search for other works by this author on: GSW Google Scholar David R. Pevear; David R. Pevear 2ExxonMobil Upstream Research Company, Houston, Texas 77252-2189, USA Search for other works by this author on: GSW Google Scholar Chris M. Hall; Chris M. Hall 3Department of Geological Sciences, University of Michigan, Ann Arbor, Michigan 48109, USA Search for other works by this author on: GSW Google Scholar John Solum John Solum 4Department of Geological Sciences, University of Michigan, Ann Arbor, Michigan 48109, USA, and U.S. Geological Survey, Earthquake Hazards Team, Menlo Park, California 94025, USA Search for other works by this author on: GSW Google Scholar Geology (2006) 34 (10): 837–840. https://doi.org/10.1130/G22610.1 Article history received: 17 Jan 2006 rev-recd: 02 May 2006 accepted: 09 May 2006 first online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Ben A. van der Pluijm, Peter J. Vrolijk, David R. Pevear, Chris M. Hall, John Solum; Fault dating in the Canadian Rocky Mountains: Evidence for late Cretaceous and early Eocene orogenic pulses. Geology 2006;; 34 (10): 837–840. doi: https://doi.org/10.1130/G22610.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Fault rocks from the classic Rocky Mountain foreland fold-and-thrust belt in southwestern Canada were dated by Ar analysis of clay grain-size fractions. Using X-ray diffraction quantification of the detrital and authigenic component of each fraction, these determinations give ages for individual faults in the area (illite age analysis). The resulting ages cluster around 72 and 52 Ma (here called the Rundle and McConnell pulses, respectively), challenging the traditional view of gradual forward progression of faulting and thrust-belt history of the area. The recognition of spatially and temporally restricted deformation episodes offers field support for theoretical models of critically stressed wedges, which result in geologically reasonable strain rates for the area. In addition to regional considerations, this study highlights the potential of direct dating of shallow fault rocks for our understanding of upper-crustal kinematics and regional tectonic analysis of ancient orogens. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2124372616 date "2006-01-01" @default.
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• W2124372616 title "Fault dating in the Canadian Rocky Mountains: Evidence for late Cretaceous and early Eocene orogenic pulses" @default.
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