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• W2760838739 abstract "Research Article| October 02, 2017 Sulfur release from main-phase Columbia River Basalt eruptions Klarissa N. Davis; Klarissa N. Davis 1School of the Environment, Washington State University, Pullman, Washington 99164, USA Search for other works by this author on: GSW Google Scholar John A. Wolff; John A. Wolff 1School of the Environment, Washington State University, Pullman, Washington 99164, USA Search for other works by this author on: GSW Google Scholar Michael C. Rowe; Michael C. Rowe 2School of Environment, University of Auckland, Auckland 1010, New Zealand Search for other works by this author on: GSW Google Scholar Owen K. Neill Owen K. Neill 1School of the Environment, Washington State University, Pullman, Washington 99164, USA Search for other works by this author on: GSW Google Scholar Author and Article Information Klarissa N. Davis 1School of the Environment, Washington State University, Pullman, Washington 99164, USA John A. Wolff 1School of the Environment, Washington State University, Pullman, Washington 99164, USA Michael C. Rowe 2School of Environment, University of Auckland, Auckland 1010, New Zealand Owen K. Neill 1School of the Environment, Washington State University, Pullman, Washington 99164, USA Publisher: Geological Society of America Received: 01 Jun 2017 Revision Received: 11 Aug 2017 Accepted: 18 Aug 2017 First Online: 02 Oct 2017 Online Issn: 1943-2682 Print Issn: 0091-7613 © 2017 Geological Society of America Geology (2017) 45 (11): 1043–1046. https://doi.org/10.1130/G39371.1 Article history Received: 01 Jun 2017 Revision Received: 11 Aug 2017 Accepted: 18 Aug 2017 First Online: 02 Oct 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Klarissa N. Davis, John A. Wolff, Michael C. Rowe, Owen K. Neill; Sulfur release from main-phase Columbia River Basalt eruptions. Geology 2017;; 45 (11): 1043–1046. doi: https://doi.org/10.1130/G39371.1 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 The Columbia River Basalt Group (western United States) is Earth’s youngest and best-studied flood basalt province, but attempts to link it with mid-Miocene global change have proven elusive. Part of the difficulty lies in a lack of comprehensive data for volatile emissions from the most intense main phase of activity. We present measurements of sulfur contents in magmas that erupted to form the Wapshilla Ridge Member and associated units of the Grande Ronde Basalt, the most voluminous portion of the Columbia River Basalt Group, erupted at the time of peak magma flux. We sampled melt inclusions and host glasses preserved in near-vent phreatomagmatic deposits associated with the voluminous lavas. Sulfur contents of melt inclusions range up to 0.19 wt% S, while host glasses are variably degassed with 0.01–0.13 wt% S. Incomplete degassing of glassy lapilli is attributed to phreatomagmatic quenching in the vent. The magmatic S contents in the very voluminous (∼40,000 km3) Wapshilla Ridge Member scale up to 242–305 Gt SO2 release to the atmosphere over a maximum time period of 94 k.y. The time of the eruption is close to that of a global temperature drop near the peak of the Miocene Climatic Optimum, but refinement of eruption tempo is needed before a cause-and-effect relation can be established. 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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• W2760838739 date "2017-10-02" @default.
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• W2760838739 title "Sulfur release from main-phase Columbia River Basalt eruptions" @default.
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