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• W2170569840 abstract "Research Article| January 01, 2006 Dissected hydrologic system at the Grand Canyon: Interaction between deeply derived fluids and plateau aquifer waters in modern springs and travertine Laura J. Crossey; Laura J. Crossey 1 Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico 87131, USA Search for other works by this author on: GSW Google Scholar Tobias P. Fischer; Tobias P. Fischer 1 Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico 87131, USA Search for other works by this author on: GSW Google Scholar P. Jonathan Patchett; P. Jonathan Patchett 2Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA Search for other works by this author on: GSW Google Scholar Karl E. Karlstrom; Karl E. Karlstrom 3Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico 87131, USA Search for other works by this author on: GSW Google Scholar David R. Hilton; David R. Hilton 4Geosciences Research Division, Scripps Institution of Oceanography, La Jolla, California 92093, USA Search for other works by this author on: GSW Google Scholar Dennis L. Newell; Dennis L. Newell 5Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico 87131, USA Search for other works by this author on: GSW Google Scholar Peter Huntoon; Peter Huntoon 6P.O. Box 60850, Boulder City, Nevada 89006, USA Search for other works by this author on: GSW Google Scholar Amanda C. Reynolds; Amanda C. Reynolds 7Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA Search for other works by this author on: GSW Google Scholar Goverdina A.M. de Leeuw Goverdina A.M. de Leeuw 8Geosciences Research Division, Scripps Institution of Oceanography, La Jolla, California 92093, USA Search for other works by this author on: GSW Google Scholar Author and Article Information Laura J. Crossey 1 Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico 87131, USA Tobias P. Fischer 1 Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico 87131, USA P. Jonathan Patchett 2Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA Karl E. Karlstrom 3Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico 87131, USA David R. Hilton 4Geosciences Research Division, Scripps Institution of Oceanography, La Jolla, California 92093, USA Dennis L. Newell 5Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico 87131, USA Peter Huntoon 6P.O. Box 60850, Boulder City, Nevada 89006, USA Amanda C. Reynolds 7Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA Goverdina A.M. de Leeuw 8Geosciences Research Division, Scripps Institution of Oceanography, La Jolla, California 92093, USA Publisher: Geological Society of America Received: 22 Jul 2005 Revision Received: 31 Aug 2005 Accepted: 03 Sep 2005 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (2006) 34 (1): 25–28. https://doi.org/10.1130/G22057.1 Article history Received: 22 Jul 2005 Revision Received: 31 Aug 2005 Accepted: 03 Sep 2005 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Laura J. Crossey, Tobias P. Fischer, P. Jonathan Patchett, Karl E. Karlstrom, David R. Hilton, Dennis L. Newell, Peter Huntoon, Amanda C. Reynolds, Goverdina A.M. de Leeuw; Dissected hydrologic system at the Grand Canyon: Interaction between deeply derived fluids and plateau aquifer waters in modern springs and travertine. Geology 2006;; 34 (1): 25–28. doi: https://doi.org/10.1130/G22057.1 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 Geochemical study of water and gas discharging from the deeply incised aquifer system at the Grand Canyon, Arizona, provides a paradigm for understanding complex groundwater mixing phenomena, and Quaternary travertines deposited from cool springs provide a paleohydrologic record of this mixing. Geochemical data show that springs have marked compositional variability: those associated with active travertine accumulations (deeply derived endogenic waters) are more saline, richer in CO2, and elevated in 87Sr/86Sr relative to springs derived dominantly from surface recharge of plateau aquifers (epigenic waters). Endogenic waters and associated travertine are preferentially located along basement-penetrating faults. We propose a model whereby deeply derived fluids are conveyed upward via both magmatism and seismicity. Our model is supported by: (1) gas analyses from spring waters with high He/Ar and He/N2 and 3He/4He ratios indicating the presence of mantle-derived He; (2) large volumes of travertine and CO2-rich gases in springs recording high CO2 fluxes; and (3) 87Sr/86Sr in these springs that indicate circulation of waters through Precambrian basement. Geochemical trends are explained by mixing of epigenic waters of the Colorado Plateau aquifers with different endogenic end-member waters in different tectonic subprovinces. Endogenic waters are volumetrically minor but have significant effects on water chemistry. They are an important and largely unrecognized component of the hydrogeochemistry and neotectonics of the southwestern United States. 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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• W2170569840 title "Dissected hydrologic system at the Grand Canyon: Interaction between deeply derived fluids and plateau aquifer waters in modern springs and travertine" @default.
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