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• W1979071779 abstract "Research Article| July 01, 2011 Eolian dynamics and sediment mixing in the Gran Desierto, Mexico, determined from thermal infrared spectroscopy and remote-sensing data Stephen Scheidt; Stephen Scheidt † 1Department of Geology and Planetary Science, University of Pittsburgh, SRCC 200, 4107 O'Hara Street, Pittsburgh, Pennsylvania 15260, USA2Desert Research Institute, 2215 Raggio Parkway, Reno, Nevada 89512, USA †sscheidt77@gmail.com Search for other works by this author on: GSW Google Scholar Nicholas Lancaster; Nicholas Lancaster 2Desert Research Institute, 2215 Raggio Parkway, Reno, Nevada 89512, USA Search for other works by this author on: GSW Google Scholar Michael Ramsey Michael Ramsey 1Department of Geology and Planetary Science, University of Pittsburgh, SRCC 200, 4107 O'Hara Street, Pittsburgh, Pennsylvania 15260, USA Search for other works by this author on: GSW Google Scholar Author and Article Information Stephen Scheidt † 1Department of Geology and Planetary Science, University of Pittsburgh, SRCC 200, 4107 O'Hara Street, Pittsburgh, Pennsylvania 15260, USA2Desert Research Institute, 2215 Raggio Parkway, Reno, Nevada 89512, USA Nicholas Lancaster 2Desert Research Institute, 2215 Raggio Parkway, Reno, Nevada 89512, USA Michael Ramsey 1Department of Geology and Planetary Science, University of Pittsburgh, SRCC 200, 4107 O'Hara Street, Pittsburgh, Pennsylvania 15260, USA †sscheidt77@gmail.com Publisher: Geological Society of America Received: 26 May 2010 Revision Received: 08 Sep 2010 Accepted: 24 Sep 2010 First Online: 08 Mar 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 © 2011 Geological Society of America GSA Bulletin (2011) 123 (7-8): 1628–1644. https://doi.org/10.1130/B30338.1 Article history Received: 26 May 2010 Revision Received: 08 Sep 2010 Accepted: 24 Sep 2010 First Online: 08 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Stephen Scheidt, Nicholas Lancaster, Michael Ramsey; Eolian dynamics and sediment mixing in the Gran Desierto, Mexico, determined from thermal infrared spectroscopy and remote-sensing data. GSA Bulletin 2011;; 123 (7-8): 1628–1644. doi: https://doi.org/10.1130/B30338.1 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 SocietyGSA Bulletin Search Advanced Search Abstract The Gran Desierto dune field is only partially composed of quartz-rich sands from the ancestral Colorado River. Local sources have been previously underestimated as a major source of sand because previous remote-sensing studies were limited in their capability to detect silicate minerals. Compositions of sands were evaluated in this study using a combination of laboratory thermal emission spectroscopy and thermal remote-sensing data acquired from the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) instrument. The spatial interpolation of sample compositions allowed visualization of the sand transport pathways from feldspar-rich local sources by revealing gradients of composition between the dune field and surrounding local sources. The laboratory data were comparable to the remote-sensing retrievals of quartz and feldspar abundance. The mineralogical maturity of the Desierto dunes could be determined by the quartz/feldspar ratio, therefore providing a context for understanding the provenance of the Gran Desierto in relation to other Mojave and Sonoran dune fields. The composition of a previously undescribed group of dunes east of the Pinacate, the Sonoyta dunes, was measured as higher in potassium feldspar relative to the rest of the dune field. The composition of Sonoyta dunes is characteristic of other Mojave dune fields, which are more isolated near local feldspar-rich sources. South of the Pinacate, quartz-rich sand from the west admixes with feldspar-rich sand from the Sonoyta dunes to the east. The northern margin of the Gran Desierto is similarly enriched in feldspar from alluvial fans, and the coastal sand is influenced by carbonate sand that does not appear to survive transport to the inland dunes. 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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• W1979071779 date "2011-02-04" @default.
• W1979071779 modified "2023-10-18" @default.
• W1979071779 title "Eolian dynamics and sediment mixing in the Gran Desierto, Mexico, determined from thermal infrared spectroscopy and remote-sensing data" @default.
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• W1979071779 doi "https://doi.org/10.1130/b30338.1" @default.
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