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• W2155879931 abstract "Research Article| December 01, 2006 Constraining the timing and migration of collisional tectonics in the Damara Belt, Namibia: U-Pb zircon ages for the syntectonic Salem-type Stinkbank granite Shannon D. Johnson; Shannon D. Johnson Department of Geology, University of Stellenbosch, Private Bag X1, Matieland 7602, South Africa, Present address: Martha Mine, Newmont Waihi Gold Ltd., PO Box 190, Waihi, New Zealand e-mail: Shannon.Johnson@Newmont.com corresponding author: e-mail: akisters@sun.ac.za Search for other works by this author on: GSW Google Scholar Marc Poujol; Marc Poujol Facility for Isotopic and Elemental Determination – Memorial University of Newfoundland, 300 Prince Philip Drive, St John’s, NL, CANADA A1B 3X5., e-mail: mpoujol@esd.mun.can Search for other works by this author on: GSW Google Scholar Alexander F.M. Kisters Alexander F.M. Kisters Department of Geology, University of Stellenbosch, Private Bag X1, Matieland 7602, South Africa Search for other works by this author on: GSW Google Scholar Author and Article Information Shannon D. Johnson Department of Geology, University of Stellenbosch, Private Bag X1, Matieland 7602, South Africa, Present address: Martha Mine, Newmont Waihi Gold Ltd., PO Box 190, Waihi, New Zealand e-mail: Shannon.Johnson@Newmont.com Marc Poujol Facility for Isotopic and Elemental Determination – Memorial University of Newfoundland, 300 Prince Philip Drive, St John’s, NL, CANADA A1B 3X5., e-mail: mpoujol@esd.mun.can Alexander F.M. Kisters Department of Geology, University of Stellenbosch, Private Bag X1, Matieland 7602, South Africa corresponding author: e-mail: akisters@sun.ac.za Publisher: Geological Society of South Africa First Online: 09 Mar 2017 Online ISSN: 1996-8590 Print ISSN: 1012-0750 © 2006 Geological Society of South Africa South African Journal of Geology (2006) 109 (4): 611–624. https://doi.org/10.2113/gssajg.109.4.611 Article history 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 Shannon D. Johnson, Marc Poujol, Alexander F.M. Kisters; Constraining the timing and migration of collisional tectonics in the Damara Belt, Namibia: U-Pb zircon ages for the syntectonic Salem-type Stinkbank granite. South African Journal of Geology 2006;; 109 (4): 611–624. doi: https://doi.org/10.2113/gssajg.109.4.611 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 SocietySouth African Journal of Geology Search Advanced Search Abstract A U-Pb zircon LAM-ICP-MS age of 549 ± 11 Ma from the Stinkbank granite in the south Central Zone of the Damara belt represents the first robust age for the crystallization of a member of the regionally widespread suite of syntectonic Salem-type granites. This age confirms previous assertions that suggest that the main phase of crustal shortening related to the collision between the Congo and Kalahari Cratrons occurred between 550 and ~540 Ma in the south Central Zone, the leading edge of the Congo Craton. Ages from syntectonic granites reported in the literature from the north Central and the Northern Zone record progressively younger ages of ~530 to ~515 Ma and late-stage folding in the Northern Zone is suggested to have occurred between ~510 to ~500 Ma. The younging of ages that date the main collisional phase towards the north is interpreted to track the northward propagation of the deformation and metamorphic front from the main suture zone to the northern foreland of the Damara belt. Geochronological data are sparse, and the lack of detailed structural data precludes the retrodeformation of the fold-and-thrust belt along this 250 km long section. However, the age brackets suggest a migration of the orogenic front at a rate of at least 5 to 7 mm/a, but more likely in the order of several centimetre per year, if the internal strain is removed. 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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