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• W2058704553 abstract "Research Article| March 01, 2009 Evolution of the northern Cordilleran foreland basin during the middle Cretaceous Yongtai Yang; Yongtai Yang † 1Department of Geology, University of Toronto, 22 Russell Street, Toronto, Ontario M5S 3B1, Canada †E-mail: yongtai.yang@utoronto.ca Search for other works by this author on: GSW Google Scholar Andrew D. Miall Andrew D. Miall 1Department of Geology, University of Toronto, 22 Russell Street, Toronto, Ontario M5S 3B1, Canada Search for other works by this author on: GSW Google Scholar GSA Bulletin (2009) 121 (3-4): 483–501. https://doi.org/10.1130/B26374.1 Article history received: 19 Nov 2007 rev-recd: 12 Jun 2008 accepted: 18 Jun 2008 first online: 02 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 Yongtai Yang, Andrew D. Miall; Evolution of the northern Cordilleran foreland basin during the middle Cretaceous. GSA Bulletin 2009;; 121 (3-4): 483–501. doi: https://doi.org/10.1130/B26374.1 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 SocietyGSA Bulletin Search Advanced Search Abstract A detailed study of the middle–late Cenomanian Belle Fourche Formation in southern Alberta helps to elucidate the evolution of the Cordilleran foreland basin during the middle Cretaceous. By combining isopach data from the study area with previously published research on middle Cretaceous stratigraphy in adjacent areas of northern Alberta and Montana, it is possible to define the position of the proximal foredeep, fore-bulge, and backbulge depozones from late Albian to Cenomanian time.The foredeep probably lay to the west of the present fold-thrust belt in western Montana from the late Albian to middle Cenomanian, with the forebulge extending northwestward through the northwest corner of Wyoming and curving northeastward through the present-day location of Calgary. Thick Dunvegan deposits (middle Cenomanian) of northwestern Alberta are interpreted as foredeep deposits. Palinspastic reconstruction of the southern Rocky Mountains of Alberta is consistent with a location of the foredeep within the area of the present fold-thrust belt.At the end of the middle Cenomanian the forebulge retreated westward within Alberta, defining a nearly straight northwest-southeast trend through the present position of the Foothills and Front Ranges of Alberta and northwestern Montana. The change in trend of the foreland basin at the end of the middle Cenomanian may reflect the change of convergence vectors along the western margin of North America during the middle Cretaceous. 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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• W2058704553 title "Evolution of the northern Cordilleran foreland basin during the middle Cretaceous" @default.
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