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- W2088646714 abstract "Research Article| April 01, 1985 Evidence for Late Cretaceous crustal thinning in the Santa Rosa mylonite zone, southern California Bradley G. Erskine; Bradley G. Erskine 1Department of Geology and Geophysics, University of California, Berkeley, California 94720 Search for other works by this author on: GSW Google Scholar H.-R. Wenk H.-R. Wenk 1Department of Geology and Geophysics, University of California, Berkeley, California 94720 Search for other works by this author on: GSW Google Scholar Author and Article Information Bradley G. Erskine 1Department of Geology and Geophysics, University of California, Berkeley, California 94720 H.-R. Wenk 1Department of Geology and Geophysics, University of California, Berkeley, California 94720 Publisher: Geological Society of America First Online: 01 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1985) 13 (4): 274–277. https://doi.org/10.1130/0091-7613(1985)13<274:EFLCCT>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 Email Permissions Search Site Citation Bradley G. Erskine, H.-R. Wenk; Evidence for Late Cretaceous crustal thinning in the Santa Rosa mylonite zone, southern California. Geology 1985;; 13 (4): 274–277. doi: https://doi.org/10.1130/0091-7613(1985)13<274:EFLCCT>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 The Santa Rosa mylonite zone is part of a 100-km-long belt of deformation along the eastern margin of the northern Peninsular Ranges batholith, southern California. In the northern Santa Rosa Mountains, complexly deformed mylonitic plutonic and metasedimentary tectonites are cut by a stacked sequence of five low-angle faults. Evidence from field relationships and the analysis of minor structures, microstructures, and textures (preferred orientation) suggest that the coaxial component of deformation (“pure shear”) dominated over a noncoaxial (“simple shear”) component. It is proposed that mylonitic deformation and low-angle faulting, which appear to be kinematically associated, are the result of Late Cretaceous extension and thinning of the continental margin. 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." @default.
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- W2088646714 title "Evidence for Late Cretaceous crustal thinning in the Santa Rosa mylonite zone, southern California" @default.
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