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• W2268964669 abstract "Research Article| September 01, 2015 Determining vorticity axes from grain-scale dispersion of crystallographic orientations Zachary D. Michels; Zachary D. Michels * 1Department of Geoscience, University of Wisconsin–Madison, 1215 West Dayton Street, Madison, Wisconsin 53706, USA *E-mail: zmichels@wisc.edu Search for other works by this author on: GSW Google Scholar Seth C. Kruckenberg; Seth C. Kruckenberg 2Department of Earth and Environmental Sciences, Boston College, 140 Commonwealth Avenue, Chestnut Hill, Massachusetts 02467, USA Search for other works by this author on: GSW Google Scholar Joshua R. Davis; Joshua R. Davis 3Department of Mathematics and Statistics, Carleton College, One North College Street, Northfield, Minnesota 55057, USA Search for other works by this author on: GSW Google Scholar Basil Tikoff Basil Tikoff 1Department of Geoscience, University of Wisconsin–Madison, 1215 West Dayton Street, Madison, Wisconsin 53706, USA Search for other works by this author on: GSW Google Scholar Author and Article Information Zachary D. Michels * 1Department of Geoscience, University of Wisconsin–Madison, 1215 West Dayton Street, Madison, Wisconsin 53706, USA Seth C. Kruckenberg 2Department of Earth and Environmental Sciences, Boston College, 140 Commonwealth Avenue, Chestnut Hill, Massachusetts 02467, USA Joshua R. Davis 3Department of Mathematics and Statistics, Carleton College, One North College Street, Northfield, Minnesota 55057, USA Basil Tikoff 1Department of Geoscience, University of Wisconsin–Madison, 1215 West Dayton Street, Madison, Wisconsin 53706, USA *E-mail: zmichels@wisc.edu Publisher: Geological Society of America Received: 08 Apr 2015 Revision Received: 29 Jun 2015 Accepted: 02 Jul 2015 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2015 Geological Society of America Geology (2015) 43 (9): 803–806. https://doi.org/10.1130/G36868.1 Article history Received: 08 Apr 2015 Revision Received: 29 Jun 2015 Accepted: 02 Jul 2015 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 Zachary D. Michels, Seth C. Kruckenberg, Joshua R. Davis, Basil Tikoff; Determining vorticity axes from grain-scale dispersion of crystallographic orientations. Geology 2015;; 43 (9): 803–806. doi: https://doi.org/10.1130/G36868.1 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 Kinematic shear sense indicators are critical tools for tectonic interpretation of shear zones. The appropriate plane in which to interpret shear sense indicators is the vorticity normal surface, which is often inferred using fabric (foliation, lineation) orientation. Strain modeling, however, suggests that such fabrics can be unreliable for determining a kinematic framework. We demonstrate the application of a new quantitative method, crystallographic vorticity axis (CVA) analysis, that utilizes rotation statistics to calculate dispersion axes from crystallographic orientations at the grain scale. We apply CVA analysis to samples from three shear zones that exhibit distinct kinematics and deformation geometries. In all cases, the aggregate of calculated grain-scale dispersion axes yields a preferred axis of crystallographic vorticity at the specimen scale that is coincident with the independently determined bulk vorticity axis. This new method allows the position of vorticity axes to be evaluated independently of foliation and lineation information, and without assumptions about the kinematics of deformation. 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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• W2268964669 title "Determining vorticity axes from grain-scale dispersion of crystallographic orientations" @default.
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