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• W2560097856 abstract "Research Article| February 01, 2017 Tidal rhythmites in the southern Bouse Formation as evidence for post-Miocene uplift of the lower Colorado River corridor Brennan O’Connell; Brennan O’Connell Department of Earth Sciences, University of Oregon, Eugene, Oregon 97403, USA Search for other works by this author on: GSW Google Scholar Rebecca J. Dorsey; Rebecca J. Dorsey Department of Earth Sciences, University of Oregon, Eugene, Oregon 97403, USA Search for other works by this author on: GSW Google Scholar Eugene D. Humphreys Eugene D. Humphreys Department of Earth Sciences, University of Oregon, Eugene, Oregon 97403, USA Search for other works by this author on: GSW Google Scholar Author and Article Information Brennan O’Connell Department of Earth Sciences, University of Oregon, Eugene, Oregon 97403, USA Rebecca J. Dorsey Department of Earth Sciences, University of Oregon, Eugene, Oregon 97403, USA Eugene D. Humphreys Department of Earth Sciences, University of Oregon, Eugene, Oregon 97403, USA Publisher: Geological Society of America Received: 15 Jul 2016 Revision Received: 25 Oct 2016 Accepted: 25 Oct 2016 First Online: 02 Jun 2017 Online Issn: 1943-2682 Print Issn: 0091-7613 © 2016 Geological Society of America Geology (2017) 45 (2): 99–102. https://doi.org/10.1130/G38608.1 Article history Received: 15 Jul 2016 Revision Received: 25 Oct 2016 Accepted: 25 Oct 2016 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 Brennan O’Connell, Rebecca J. Dorsey, Eugene D. Humphreys; Tidal rhythmites in the southern Bouse Formation as evidence for post-Miocene uplift of the lower Colorado River corridor. Geology 2017;; 45 (2): 99–102. doi: https://doi.org/10.1130/G38608.1 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 Uncertainty over depositional paleoenvironments of the upper Miocene to lower Pliocene Bouse Formation obscures our understanding of the timing and magnitude of regional uplift as well as the conditions and processes that were active during integration and early evolution of the Colorado River (western United States). This paper presents new sedimentologic and quantitative evidence for a strong tidal influence on deposition of the basal carbonate member of the southern Bouse Formation. Lithofacies with tidal sedimentary structures include lime mudstone with reed and grass imprints; heterolithic facies with horizontal, flaser, wavy, and lenticular bedding; and cross-bedded grainstone with sigmoidal bundles, reactivation surfaces, and complex bedding. Systematic alternation of relatively thick and thin layers records a predominantly semidiurnal mixed-tidal depositional environment, and Fourier analysis highlights the cyclic, non-random nature of layer-thickness trends. These observations provide evidence that the southern Bouse Formation accumulated in a pre–Colorado River tide-dominated marine setting at the north end of the Gulf of California. Deposition at sea level requires ∼330 m of uplift in the lower Colorado River and western Colorado Plateau region during the past ∼5.0 m.y. 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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• W2560097856 title "Tidal rhythmites in the southern Bouse Formation as evidence for post-Miocene uplift of the lower Colorado River corridor" @default.
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