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• W2013374002 abstract "Research Article| January 01, 2006 Timing of Cenozoic volcanism and Basin and Range extension in northwestern Nevada: New constraints from the northern Pine Forest Range Joseph P. Colgan; Joseph P. Colgan 1Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305-2115, USA Search for other works by this author on: GSW Google Scholar Trevor A. Dumitru; Trevor A. Dumitru 1Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305-2115, USA Search for other works by this author on: GSW Google Scholar Michael McWilliams; Michael McWilliams 1Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305-2115, USA Search for other works by this author on: GSW Google Scholar Elizabeth L. Miller Elizabeth L. Miller 1Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305-2115, USA Search for other works by this author on: GSW Google Scholar Author and Article Information Joseph P. Colgan 1Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305-2115, USA Trevor A. Dumitru 1Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305-2115, USA Michael McWilliams 1Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305-2115, USA Elizabeth L. Miller 1Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305-2115, USA Publisher: Geological Society of America Received: 19 Jul 2004 Revision Received: 09 Apr 2005 Accepted: 04 May 2005 First Online: 08 Mar 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Geological Society of America GSA Bulletin (2006) 118 (1-2): 126–139. https://doi.org/10.1130/B25681.1 Article history Received: 19 Jul 2004 Revision Received: 09 Apr 2005 Accepted: 04 May 2005 First Online: 08 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Joseph P. Colgan, Trevor A. Dumitru, Michael McWilliams, Elizabeth L. Miller; Timing of Cenozoic volcanism and Basin and Range extension in northwestern Nevada: New constraints from the northern Pine Forest Range. GSA Bulletin 2006;; 118 (1-2): 126–139. doi: https://doi.org/10.1130/B25681.1 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 Eocene–middle Miocene volcanic rocks in the northern Pine Forest Range, Nevada, are ideally situated for reconstructing the timing and style of volcanism and extensional faulting in the northwesternmost part of the Basin and Range province. A conformable sequence of Cenozoic volcanic and sedimentary strata in the northern Pine Forest Range dips ∼30°W, and 11 new 40Ar/39Ar ages from this sequence define 3 major episodes of volcanic activity. Pre-Tertiary basement and older (ca. 38 Ma) Tertiary intrusive rocks are overlain unconformably by Oligocene (ca. 30–23 Ma) basalt flows and dacitic to rhyolitic ash-flow tuffs interbedded with fine-grained tuffaceous sedimentary rocks. Oligocene rocks are overlain by ∼550 m of ca. 17–16 Ma basalt flows equivalent to the Steens Basalt in southern Oregon, and basalt flows are capped by a thin 16.3 Ma ignimbrite that likely is correlative with either the Idaho Canyon Tuff or the Tuff of Oregon Canyon. The northern Pine Forest Range is bounded to the east by a major down-to-the-east normal fault that dips ∼40°E with well-developed fault striations indicative of dip-slip motion. This fault initiated at an angle of ∼70° and was rotated ∼30° during uplift of the range. A suite of 17 apatite fission-track ages from the Pine Forest footwall block demonstrates that exhumation, uplift, and slip on the range-bounding fault began ca. 12–11 Ma and continued until at least 7 Ma, with moderate slip since then. The Pine Forest Range did not undergo significant extension before or during peak Oligocene and Miocene volcanism, and similar geologic relationships in nearby ranges suggest that a larger region of northwestern Nevada was also little extended during this interval. Basin and Range faulting in northwestern Nevada appears to have begun no earlier than 12 Ma, making it distinctly younger than deformation in much of central and southern Nevada, where peak extension occurred in the middle Miocene or earlier. 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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• W2013374002 title "Timing of Cenozoic volcanism and Basin and Range extension in northwestern Nevada: New constraints from the northern Pine Forest Range" @default.
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