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• W2014169648 abstract "Research Article| August 01, 2008 A Geophysical Investigation of Shallow Deformation Along an Anomalous Section of the Wasatch Fault Zone, Utah, USA J.H. MCBRIDE; J.H. MCBRIDE 1Department of Geological Sciences, Brigham Young University, P.O. Box 24606, Provo, Utah 84602 Search for other works by this author on: GSW Google Scholar W.J. STEPHENSON; W.J. STEPHENSON 2U.S. Geological Survey, Denver Federal Center MS 966 Box 25046, Denver, Colorado 80225 Search for other works by this author on: GSW Google Scholar T.J. THOMPSON; T.J. THOMPSON 3GeoStrata, LLC, 781 West 14600 South, Bluffdale, Utah 84065 Search for other works by this author on: GSW Google Scholar M.P. HARPER; M.P. HARPER 3GeoStrata, LLC, 781 West 14600 South, Bluffdale, Utah 84065 Search for other works by this author on: GSW Google Scholar A.A. EIPERT; A.A. EIPERT 3GeoStrata, LLC, 781 West 14600 South, Bluffdale, Utah 84065 Search for other works by this author on: GSW Google Scholar J.C. HOOPES; J.C. HOOPES 4Department of Geological Sciences, Brigham Young University, P.O. Box 24606, Provo, Utah 84602 Search for other works by this author on: GSW Google Scholar D.G. TINGEY; D.G. TINGEY 4Department of Geological Sciences, Brigham Young University, P.O. Box 24606, Provo, Utah 84602 Search for other works by this author on: GSW Google Scholar R.W. KEACH, II; R.W. KEACH, II 4Department of Geological Sciences, Brigham Young University, P.O. Box 24606, Provo, Utah 84602 Search for other works by this author on: GSW Google Scholar A.O. OKOJIE-AYORO; A.O. OKOJIE-AYORO 4Department of Geological Sciences, Brigham Young University, P.O. Box 24606, Provo, Utah 84602 Search for other works by this author on: GSW Google Scholar K.L. GUNDERSON; K.L. GUNDERSON 4Department of Geological Sciences, Brigham Young University, P.O. Box 24606, Provo, Utah 84602 Search for other works by this author on: GSW Google Scholar C.D. MEIROVITZ; C.D. MEIROVITZ 4Department of Geological Sciences, Brigham Young University, P.O. Box 24606, Provo, Utah 84602 Search for other works by this author on: GSW Google Scholar T.C. HICKS; T.C. HICKS 4Department of Geological Sciences, Brigham Young University, P.O. Box 24606, Provo, Utah 84602 Search for other works by this author on: GSW Google Scholar C.J. SPENCER; C.J. SPENCER 4Department of Geological Sciences, Brigham Young University, P.O. Box 24606, Provo, Utah 84602 Search for other works by this author on: GSW Google Scholar J.R. YAEDE; J.R. YAEDE 4Department of Geological Sciences, Brigham Young University, P.O. Box 24606, Provo, Utah 84602 Search for other works by this author on: GSW Google Scholar D.M. WORLEY D.M. WORLEY 5U.S. Geological Survey, Denver Federal Center MS 966 Box 25046, Denver, Colorado 80225 Search for other works by this author on: GSW Google Scholar Author and Article Information J.H. MCBRIDE 1Department of Geological Sciences, Brigham Young University, P.O. Box 24606, Provo, Utah 84602 W.J. STEPHENSON 2U.S. Geological Survey, Denver Federal Center MS 966 Box 25046, Denver, Colorado 80225 T.J. THOMPSON 3GeoStrata, LLC, 781 West 14600 South, Bluffdale, Utah 84065 M.P. HARPER 3GeoStrata, LLC, 781 West 14600 South, Bluffdale, Utah 84065 A.A. EIPERT 3GeoStrata, LLC, 781 West 14600 South, Bluffdale, Utah 84065 J.C. HOOPES 4Department of Geological Sciences, Brigham Young University, P.O. Box 24606, Provo, Utah 84602 D.G. TINGEY 4Department of Geological Sciences, Brigham Young University, P.O. Box 24606, Provo, Utah 84602 R.W. KEACH, II 4Department of Geological Sciences, Brigham Young University, P.O. Box 24606, Provo, Utah 84602 A.O. OKOJIE-AYORO 4Department of Geological Sciences, Brigham Young University, P.O. Box 24606, Provo, Utah 84602 K.L. GUNDERSON 4Department of Geological Sciences, Brigham Young University, P.O. Box 24606, Provo, Utah 84602 C.D. MEIROVITZ 4Department of Geological Sciences, Brigham Young University, P.O. Box 24606, Provo, Utah 84602 T.C. HICKS 4Department of Geological Sciences, Brigham Young University, P.O. Box 24606, Provo, Utah 84602 C.J. SPENCER 4Department of Geological Sciences, Brigham Young University, P.O. Box 24606, Provo, Utah 84602 J.R. YAEDE 4Department of Geological Sciences, Brigham Young University, P.O. Box 24606, Provo, Utah 84602 D.M. WORLEY 5U.S. Geological Survey, Denver Federal Center MS 966 Box 25046, Denver, Colorado 80225 Publisher: Association of Environmental & Engineering Geologists First Online: 02 Mar 2017 Online ISSN: 1558-9161 Print ISSN: 1078-7275 Copyright © 2008 © 2005 Association of Engineering Geologists Environmental & Engineering Geoscience (2008) 14 (3): 183–197. https://doi.org/10.2113/gseegeosci.14.3.183 Article history First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation J.H. MCBRIDE, W.J. STEPHENSON, T.J. THOMPSON, M.P. HARPER, A.A. EIPERT, J.C. HOOPES, D.G. TINGEY, R.W. KEACH, A.O. OKOJIE-AYORO, K.L. GUNDERSON, C.D. MEIROVITZ, T.C. HICKS, C.J. SPENCER, J.R. YAEDE, D.M. WORLEY; A Geophysical Investigation of Shallow Deformation Along an Anomalous Section of the Wasatch Fault Zone, Utah, USA. Environmental & Engineering Geoscience 2008;; 14 (3): 183–197. doi: https://doi.org/10.2113/gseegeosci.14.3.183 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 SocietyEnvironmental & Engineering Geoscience Search Advanced Search Abstract We report the results of a geophysical study of the Wasatch fault zone near the Provo and Salt Lake City segment boundary. This area is anomalous because the fault zone strikes more east-west than north-south. Vibroseis was used to record a common mid-point (CMP) profile that provides information to depths of ∼500 m. A tomographic velocity model, derived from first breaks, constrained source and receiver static corrections; this was required due to complex terrain and significant lateral velocity contrasts. The profile reveals an ∼250-m-wide graben in the hanging wall of the main fault that is associated with both synthetic and antithetic faults. Faults defined by apparent reflector offsets propagate upward toward topographic gradients. Faults mapped from a nearby trench and the seismic profile also appear to correlate with topographic alignments on LiDAR gradient maps. The faults as measured in the trench show a wide range of apparent dips, 20°–90°, and appear to steepen with depth on the seismic section. Although the fault zone is likely composed of numerous small faults, the broad asymmetric structure in the hanging wall is fairly simple and dominated by two inward-facing ruptures. Our results indicate the feasibility of mapping fault zones in rugged terrain and complex near-surface geology using low-frequency vibroseis. Further, the integration of geologic mapping and seismic reflection can extend surface observations in areas where structural deformation is obscured by poorly stratified or otherwise unmappable deposits. Therefore, the vibroseis technique, when integrated with geological information, provides constraints for assessing geologic hazards in areas of potential development. 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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