Reconciliation of San Andreas slip discrepancy by a combination of interior Basin and Range extension and transrotation near the coast

Research Article| July 01, 1997 Reconciliation of San Andreas slip discrepancy by a combination of interior Basin and Range extension and transrotation near the coast William R. Dickinson; William R. Dickinson 1Department of Geosciences, University of Arizona, Tucson, Arizona 85718 Search for other works by this author on: GSW Google Scholar Brian P. Wernicke Brian P. Wernicke 2Division of Geological and Planetary Science, California Institute of Technology, Pasadena, California 91125 Search for other works by this author on: GSW Google Scholar Geology (1997) 25 (7): 663–665. https://doi.org/10.1130/0091-7613(1997)025<0663:ROSASD>2.3.CO;2 Article history first online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation William R. Dickinson, Brian P. Wernicke; Reconciliation of San Andreas slip discrepancy by a combination of interior Basin and Range extension and transrotation near the coast. Geology 1997;; 25 (7): 663–665. doi: https://doi.org/10.1130/0091-7613(1997)025<0663:ROSASD>2.3.CO;2 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 Measurements of net translation along the Neogene San Andreas transform boundary between Pacific and North American plates, as indicated by the global correlation of sea-floor magnetic anomalies and by total Neogene displacements along strands of the onshore San Andreas fault system, differ by hundreds of kilometres. The apparent motion discrepancy is reconciled for post–mid-Miocene time if both transrotational deformation along the coastal belt of California and basin-range extension east of the Sierra Nevada are taken into account. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.