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• W2159483760 abstract "Research Article| September 01, 1994 Is the Sevier Desert reflection of west-central Utah a normal fault? Mark H. Anders; Mark H. Anders 1Department of Geological Sciences and Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York 10964-8000 Search for other works by this author on: GSW Google Scholar Nicholas Christie-Blick Nicholas Christie-Blick 1Department of Geological Sciences and Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York 10964-8000 Search for other works by this author on: GSW Google Scholar Author and Article Information Mark H. Anders 1Department of Geological Sciences and Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York 10964-8000 Nicholas Christie-Blick 1Department of Geological Sciences and Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York 10964-8000 Publisher: Geological Society of America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1994) 22 (9): 771–774. https://doi.org/10.1130/0091-7613(1994)022<0771:ITSDRO>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 MailTo Tools Icon Tools Get Permissions Search Site Citation Mark H. Anders, Nicholas Christie-Blick; Is the Sevier Desert reflection of west-central Utah a normal fault?. Geology 1994;; 22 (9): 771–774. doi: https://doi.org/10.1130/0091-7613(1994)022<0771:ITSDRO>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 A prominent west-dipping reflection that can be traced in seismic-reflection profiles over an area of 7000 km2 beneath the Sevier Desert basin of west-central Utah is generally referred to as the Sevier Desert detachment and is widely regarded as one of the best examples of an upper-crustal low-angle normal fault. The absence of evidence for fault-related deformation in drill cuttings and core from two industry boreboles that intersect this feature casts doubt on the fault interpretation. The existing interpretation is based mainly on the observation that high-angle normal faulting is restricted largely to Tertiary sedimentary and volcanic rocks above the reflection. An alternative explanation is that the high-angle faults are related to the withdrawal of early deposited lacustrine salt, which even today is as much as 2 km thick. Reevaluation of the seismic data suggests that the Sevier Desert reflection consists of two spatially and genetically distinct segments: a shallow segment here interpreted as an unconformity between Paleozoic and Tertiary strata and a fortuitously aligned deeper segment that is traceable to mid- and lower-crustal levels and that appears to represent a thrust fault related to the Cretaceous Sevier orogeny. 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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• W2159483760 title "Is the Sevier Desert reflection of west-central Utah a normal fault?" @default.
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