Reconstruction of Mid-Cenozoic Extension In
Reconstruction of MidCenozoic Extension in the Rincon Mountains Area, Southeastern Arizona, USA, and Geodynamic Implications Item Type Article Authors Spencer, Jon E.; Richard, Stephen M.; Lingrey, Steven H.; Johnson, Bradford J.; Johnson, Roy A.; Gehrels, George E. Citation Spencer, J. E., Richard, S. M., Lingrey,S. H., Johnson, B. J., Johnson, R. A., & Gehrels, G. E. (2019). Reconstruction of mid Cenozoic extension in the Rincon Mountains area, south eastern Arizona,USA, and geodynamic implications.Tectonics,38, 2338– 2357. https://doi.org/10.1029/2019TC005565 DOI 10.1029/2019tc005565 Publisher AMER GEOPHYSICAL UNION Journal TECTONICS Rights Copyright © 2019. American Geophysical Union.All Rights Reserved. Download date 10/10/2021 17:17:00 Item License http://rightsstatements.org/vocab/InC/1.0/ Version Final published version Link to Item http://hdl.handle.net/10150/634480 RESEARCH ARTICLE Reconstruction of Mid‐Cenozoic Extension in the 10.1029/2019TC005565 Rincon Mountains Area, Southeastern Arizona, Key Points: • Structural reconstruction of the San USA, and Geodynamic Implications Pedro detachment fault in Jon E. Spencer1 , Stephen M. Richard1 , Steven H. Lingrey1, Bradford J. Johnson2, southeastern Arizona indicates 34– 1 1 38 km of top‐southwest Roy A. Johnson , and George E. Gehrels displacement 1 2 • The San Pedro fault cut through Department of Geosciences, University of Arizona, Tucson, AZ, USA, Arizona Geological Survey, University of Arizona, carbonate tectonites beneath an Tucson, AZ, USA older thrust fault that formed a weak zone in the upper crust • The architecture of core complexes Abstract The Rincon Mountains metamorphic core complex, located east of Tucson, Arizona, consists may have been influenced by upper crustal weak zones inherited from of an arched footwall of foliated crystalline rocks bounded above by the generally outward dipping, older thrust faulting Oligocene‐Miocene San Pedro extensional detachment fault.
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