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• W2131090408 abstract "Research Article| March 01, 2015 Residual stress preserved in quartz from the San Andreas Fault Observatory at Depth Kai Chen; Kai Chen 1Center for Advancing Materials Performance from the Nanoscale (CAMP-Nano), State Key Laboratory for Mechanical Behavior of Materials, Xi’an Jiantong University, Xi’an, Shaanxi 710049, China Search for other works by this author on: GSW Google Scholar Martin Kunz; Martin Kunz 2Advanced Light Source, Lawrence Berkeley National Laboratory, Berkeley, California 94720, USA Search for other works by this author on: GSW Google Scholar Nobumichi Tamura; Nobumichi Tamura 2Advanced Light Source, Lawrence Berkeley National Laboratory, Berkeley, California 94720, USA Search for other works by this author on: GSW Google Scholar Hans-Rudolf Wenk Hans-Rudolf Wenk 3Earth and Planetary Science, University of California–Berkeley, Berkeley, California 94720, USA Search for other works by this author on: GSW Google Scholar Geology (2015) 43 (3): 219–222. https://doi.org/10.1130/G36443.1 Article history received: 11 Nov 2014 rev-recd: 17 Dec 2014 accepted: 18 Dec 2014 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 Kai Chen, Martin Kunz, Nobumichi Tamura, Hans-Rudolf Wenk; Residual stress preserved in quartz from the San Andreas Fault Observatory at Depth. Geology 2015;; 43 (3): 219–222. doi: https://doi.org/10.1130/G36443.1 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 We report on measurements of residual stress up to 300 MPa with a microfocused synchrotron X-ray beam in quartz fragments in a cataclasite from the damage zone of the San Andreas fault, California (USA). Samples were extracted from the San Andreas Fault Observatory at Depth drill core at a depth of 2.7 km. Stresses were derived from lattice distortions observed on Laue diffraction images. These stresses are distributed nonhomogeneously at the micron scale and are much higher than bulk-rock strengths of fault gouge, suggesting different processes at the microscopic and macroscopic scales. Our results indicate that residual lattice strain in quartz is a potential paleopiezometer to estimate stress in deformed rocks. 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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• W2131090408 title "Residual stress preserved in quartz from the San Andreas Fault Observatory at Depth" @default.
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