Research Article| June 01, 2013 A simple mechanism for mid-crustal shear zones to record surface-derived fluid signatures Tom Raimondo; Tom Raimondo * 1School of Natural and Built Environments, University of South Australia, GPO Box 2471, Adelaide, SA 5001, Australia2School of Earth and Environmental Sciences, University of Adelaide, Adelaide, SA 5005, Australia *E-mail: tom.raimondo@unisa.edu.au. Search for other works by this author on: GSW Google Scholar Chris Clark; Chris Clark 3Department of Applied Geology, Curtin University, GPO Box U1987, Perth, WA 6845, Australia Search for other works by this author on: GSW Google Scholar Martin Hand; Martin Hand 2School of Earth and Environmental Sciences, University of Adelaide, Adelaide, SA 5005, Australia Search for other works by this author on: GSW Google Scholar John Cliff; John Cliff 4Centre for Microscopy, Characterisation and Analysis, University of Western Australia, Crawley, WA 6009, Australia Search for other works by this author on: GSW Google Scholar Robert Anczkiewicz Robert Anczkiewicz 5Institute of Geological Sciences, Polish Academy of Sciences, Kraków Research Centre, Senacka 1, PL 31002 Kraków, Poland Search for other works by this author on: GSW Google Scholar Geology (2013) 41 (6): 711–714. https://doi.org/10.1130/G34043.1 Article history received: 14 Sep 2012 rev-recd: 29 Jan 2013 accepted: 30 Jan 2013 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 Tom Raimondo, Chris Clark, Martin Hand, John Cliff, Robert Anczkiewicz; A simple mechanism for mid-crustal shear zones to record surface-derived fluid signatures. Geology 2013;; 41 (6): 711–714. doi: https://doi.org/10.1130/G34043.1 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 Ion microprobe analyses of garnet porphyroblasts from three separate splays of the mid-crustal Walter-Outalpa shear zone, Curnamona Province, South Australia, indicate homogeneous δ18O values of <3‰. Integrated Lu-Hf geochronology and electron microprobe compositional mapping demonstrate that closed-system growth of these isotopically light garnets initiated as early as 531 Ma, prior to peak metamorphism and deformation during the Delamerian Orogeny (514–490 Ma). We attribute this to the prograde burial and dehydration of altered fault panels under thick sedimentary sequences during pre-orogenic basin formation. Contrary to established fluid transport models, surficial fluid signatures were not imposed at depth by large fluxes of downward-penetrating fluids, but rather by the exposure and meteoric alteration of fault rocks that were subsequently buried and reactivated as ductile shear zones. The existence of low δ18O values in deeply exhumed shear zones may therefore be indicative of fault structures that have a prior history of surface exposure, weathering, burial and re-exposure. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.