Paleomagnetic data from the Redding section of the eastern Klamath belt, northern California

Abstract

Research Article| September 01, 1983 Paleomagnetic data from the Redding section of the eastern Klamath belt, northern California Stuart W. Fagin; Stuart W. Fagin 1Department of Geologic Sciences and Institute for Geophysics, University of Texas, Austin, Texas 78712 Search for other works by this author on: GSW Google Scholar Wulf A. Gose Wulf A. Gose 1Department of Geologic Sciences and Institute for Geophysics, University of Texas, Austin, Texas 78712 Search for other works by this author on: GSW Google Scholar Geology (1983) 11 (9): 505–508. https://doi.org/10.1130/0091-7613(1983)11<505:PDFTRS>2.0.CO;2 Article history first online: 01 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 Stuart W. Fagin, Wulf A. Gose; Paleomagnetic data from the Redding section of the eastern Klamath belt, northern California. Geology 1983;; 11 (9): 505–508. doi: https://doi.org/10.1130/0091-7613(1983)11<505:PDFTRS>2.0.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 A paleomagnetic analysis of units of Devonian to Triassic age within the Redding section of the eastern Klamath Mountains indicates clockwise rotation of 83°–116° with respect to stable North America. In the kinematic model presented here, shear zones within the Franciscan Complex, with separation antithetic to the San Andreas, are used to effect this rotation. 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.