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- W2019977269 abstract "Research Article| March 01, 1990 Folding of mylonitic zones in Cordilleran metamorphic core complexes: Evidence from near the mylonitic front Stephen J. Reynolds; Stephen J. Reynolds 1Arizona Geological Survey, 845 N. Park Avenue, Tucson, Arizona 85719 Search for other works by this author on: GSW Google Scholar Gordon S. Lister Gordon S. Lister 2Department of Earth Sciences, Monash University, Melbourne, 3168 Australia Search for other works by this author on: GSW Google Scholar Author and Article Information Stephen J. Reynolds 1Arizona Geological Survey, 845 N. Park Avenue, Tucson, Arizona 85719 Gordon S. Lister 2Department of Earth Sciences, Monash University, Melbourne, 3168 Australia Publisher: Geological Society of America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1990) 18 (3): 216–219. https://doi.org/10.1130/0091-7613(1990)018<0216:FOMZIC>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 Email Permissions Search Site Citation Stephen J. Reynolds, Gordon S. Lister; Folding of mylonitic zones in Cordilleran metamorphic core complexes: Evidence from near the mylonitic front. Geology 1990;; 18 (3): 216–219. doi: https://doi.org/10.1130/0091-7613(1990)018<0216:FOMZIC>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 Metamorphic core complexes of North America are asymmetric when viewed perpendicular to the direction of tectonic transport. On one side, mylonitic fabrics and the overlying detachment fault dip gently in the direction of upper-plate transport, and the mylonitic rocks have a down-dip sense of shear. On the opposite side, the mylonitic zone rolls over to a dip opposed to the direction of upper-plate transport, diverges downward from the detachment fault, and dies out upward across a mylonitic front. New kinematic data show that the backdipping mylonitic zone in most complexes is a downfolded continuation of the main mylonitic zone. Folding of the mylonitic zone was accompanied by the formation of antithetic shear zones and occurred during the late stages of mylonitization. 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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- W2019977269 title "Folding of mylonitic zones in Cordilleran metamorphic core complexes: Evidence from near the mylonitic front" @default.
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