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• W2271594594 abstract "Research Article| October 01, 2015 Precambrian reidite discovered in shocked zircon from the Stac Fada impactite, Scotland S.M. Reddy; S.M. Reddy * 1Department of Applied Geology, Institute for Geoscience Research (TIGeR), Curtin University, GPO Box U1987, Perth, WA 6845, Australia *E-mail: s.reddy@curtin.edu.au Search for other works by this author on: GSW Google Scholar T.E. Johnson; T.E. Johnson 1Department of Applied Geology, Institute for Geoscience Research (TIGeR), Curtin University, GPO Box U1987, Perth, WA 6845, Australia Search for other works by this author on: GSW Google Scholar S. Fischer; S. Fischer 2Department of Earth and Environmental Sciences, University of St Andrews, St Andrews, Fife KY16 9AL, UK Search for other works by this author on: GSW Google Scholar W.D.A. Rickard; W.D.A. Rickard 3Department of Imaging and Applied Physics, Curtin University, GPO Box U1987, Perth, WA 6845, Australia Search for other works by this author on: GSW Google Scholar R.J.M. Taylor R.J.M. Taylor 1Department of Applied Geology, Institute for Geoscience Research (TIGeR), Curtin University, GPO Box U1987, Perth, WA 6845, Australia Search for other works by this author on: GSW Google Scholar Author and Article Information S.M. Reddy * 1Department of Applied Geology, Institute for Geoscience Research (TIGeR), Curtin University, GPO Box U1987, Perth, WA 6845, Australia T.E. Johnson 1Department of Applied Geology, Institute for Geoscience Research (TIGeR), Curtin University, GPO Box U1987, Perth, WA 6845, Australia S. Fischer 2Department of Earth and Environmental Sciences, University of St Andrews, St Andrews, Fife KY16 9AL, UK W.D.A. Rickard 3Department of Imaging and Applied Physics, Curtin University, GPO Box U1987, Perth, WA 6845, Australia R.J.M. Taylor 1Department of Applied Geology, Institute for Geoscience Research (TIGeR), Curtin University, GPO Box U1987, Perth, WA 6845, Australia *E-mail: s.reddy@curtin.edu.au Publisher: Geological Society of America Received: 15 Jun 2015 Revision Received: 02 Aug 2015 Accepted: 07 Aug 2015 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2015 Geological Society of America Geology (2015) 43 (10): 899–902. https://doi.org/10.1130/G37066.1 Article history Received: 15 Jun 2015 Revision Received: 02 Aug 2015 Accepted: 07 Aug 2015 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation S.M. Reddy, T.E. Johnson, S. Fischer, W.D.A. Rickard, R.J.M. Taylor; Precambrian reidite discovered in shocked zircon from the Stac Fada impactite, Scotland. Geology 2015;; 43 (10): 899–902. doi: https://doi.org/10.1130/G37066.1 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 Terrestrial impact events have had a profound influence on Earth’s geological, geochemical, and biological evolution. However, the record of Precambrian impacts is poorly constrained due to the dynamic nature of plate tectonics, erosion, and deposition of younger rocks that may destroy or cover the evidence. Here we report the first Precambrian occurrence of the rare mineral reidite (ZrSiO4) within grains of shocked zircon in the ca. 1.18 Ga Stac Fada Member (Stoer Group), northwestern Scotland. The reidite, preserved as <2-µm-wide lamellae, is unambiguous evidence of shock pressures in excess of ∼30 GPa and confirms the impact origin for the Stac Fada deposit. The reidite lamellae are locally deformed, and sites of deformation record its decomposition to baddeleyite (ZrO2) and amorphous silica, the first natural example of this transformation. The findings demonstrate that reidite and baddeleyite may form and be transported in high-energy ejecta without physical or chemical breakdown and are stable during sedimentary diagenesis and low-grade metamorphism. Thus, reidite may be preserved over time scales exceeding 1 b.y., establishing the use of reidite within detrital shocked zircon from Precambrian strata as a viable and valuable means of recognizing and characterizing ancient terrestrial impact events. 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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• W2271594594 title "Precambrian reidite discovered in shocked zircon from the Stac Fada impactite, Scotland" @default.
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