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• W2023941853 abstract "Research Article| September 01, 2009 Magmatic evolution of the eastern Coast Plutonic Complex, Bella Coola region, west-central British Columbia J. Brian Mahoney; J. Brian Mahoney † 1Department of Geology, University of Wisconsin–Eau Claire, 105 Garfield Avenue, Eau Claire, Wisconsin 54702-4004, USA †E-mail: mahonej@uwec.edu Search for other works by this author on: GSW Google Scholar Sarah M. Gordee; Sarah M. Gordee 1Department of Geology, University of Wisconsin–Eau Claire, 105 Garfield Avenue, Eau Claire, Wisconsin 54702-4004, USA2Department of Earth and Ocean Sciences, The University of British Columbia, 6339 Stores Road, Vancouver, BC V6T 1Z4, Canada Search for other works by this author on: GSW Google Scholar James W. Haggart; James W. Haggart 2Department of Earth and Ocean Sciences, The University of British Columbia, 6339 Stores Road, Vancouver, BC V6T 1Z4, Canada3Geological Survey of Canada, 625 Robson Street, Vancouver, BC V6B 5J3, Canada Search for other works by this author on: GSW Google Scholar Richard M. Friedman; Richard M. Friedman 2Department of Earth and Ocean Sciences, The University of British Columbia, 6339 Stores Road, Vancouver, BC V6T 1Z4, Canada Search for other works by this author on: GSW Google Scholar Larry J. Diakow; Larry J. Diakow 4British Columbia Ministry of Energy and Mines, P.O. Box 9320, Station Provincial Government, Victoria, BC V8W 9N3, Canada Search for other works by this author on: GSW Google Scholar Glenn J. Woodsworth Glenn J. Woodsworth 3Geological Survey of Canada, 625 Robson Street, Vancouver, BC V6B 5J3, Canada Search for other works by this author on: GSW Google Scholar GSA Bulletin (2009) 121 (9-10): 1362–1380. https://doi.org/10.1130/B26325.1 Article history received: 06 Sep 2007 rev-recd: 23 Oct 2008 accepted: 21 Nov 2008 first online: 02 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 J. Brian Mahoney, Sarah M. Gordee, James W. Haggart, Richard M. Friedman, Larry J. Diakow, Glenn J. Woodsworth; Magmatic evolution of the eastern Coast Plutonic Complex, Bella Coola region, west-central British Columbia. GSA Bulletin 2009;; 121 (9-10): 1362–1380. doi: https://doi.org/10.1130/B26325.1 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 eastern Coast Plutonic Complex in west-central British Columbia (51–54°N) consists of a broad belt of Jurassic to Eocene granitic to dioritic intrusive rocks that collectively represent more than 140 m.y. of nearly continuous, subduction-related magmatism. Seven distinct intrusive suites have been identified in the Bella Coola region, including, from oldest to youngest, the Howe Lake, Stick Pass, Firvale, Desire, Fougner, Big Snow, and Four Mile suites. Pre–Late Cretaceous rocks were produced by episodic subduction-related magmatism characterized by partial melting of preexisting lower-arc crust, with minimal incorporation of evolved continental material. The eastern Coast Plutonic Complex experienced a magmatic lull between ca. 110 and 95 Ma, coincident with sinistral transpression potentially linked to translational displacement of the Wrangellia-Alexander composite terranes. Crustal thickening in Late Cretaceous time (ca. 100–90 Ma), possibly due to underplating of the Wrangellia-Alexander terrane, produced a deep crustal root (>40 km) that likely extended into the eclogite transition zone. Adakitic magmas (ca. 95–67 Ma) were produced by partial melting of an amphibolitic protolith in this thickened lower-arc crust. Adakitic plutons are pre-, syn-, and postkinematic with respect to Late Cretaceous high-angle shear zones, and they are coeval and spatially associated with postkinematic two-mica granites (ca. 70–75 Ma) having a hybrid A-type geochemistry. We suggest that delamination of this dense crustal root led to voluminous magmatism, extension, and crustal exhumation in Paleocene-Eocene time. The successive intrusive events in the eastern Coast Plutonic Complex may reflect a predictable evolutionary progression common to all continental arc systems. 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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• W2023941853 date "2009-07-21" @default.
• W2023941853 modified "2023-09-26" @default.
• W2023941853 title "Magmatic evolution of the eastern Coast Plutonic Complex, Bella Coola region, west-central British Columbia" @default.
• W2023941853 cites W1610245850 @default.
• W2023941853 cites W1630322587 @default.
• W2023941853 cites W1691537565 @default.
• W2023941853 cites W1816189436 @default.
• W2023941853 cites W1967082613 @default.
• W2023941853 cites W1973871391 @default.
• W2023941853 cites W1974499954 @default.
• W2023941853 cites W1976989630 @default.
• W2023941853 cites W1977650828 @default.
• W2023941853 cites W1978765751 @default.
• W2023941853 cites W1979705656 @default.
• W2023941853 cites W1988317790 @default.
• W2023941853 cites W1991334434 @default.
• W2023941853 cites W1995971009 @default.
• W2023941853 cites W1999708461 @default.
• W2023941853 cites W2004379863 @default.
• W2023941853 cites W2007755972 @default.
• W2023941853 cites W2007902981 @default.
• W2023941853 cites W2012589759 @default.
• W2023941853 cites W2013875410 @default.
• W2023941853 cites W2013883793 @default.
• W2023941853 cites W2022017333 @default.
• W2023941853 cites W2025765909 @default.
• W2023941853 cites W2030259397 @default.
• W2023941853 cites W2030958259 @default.
• W2023941853 cites W2034144949 @default.
• W2023941853 cites W2044921168 @default.
• W2023941853 cites W2047180528 @default.
• W2023941853 cites W2049705713 @default.
• W2023941853 cites W2052011354 @default.
• W2023941853 cites W2052021185 @default.
• W2023941853 cites W2055412715 @default.
• W2023941853 cites W2057550910 @default.
• W2023941853 cites W2065030764 @default.
• W2023941853 cites W2065084016 @default.
• W2023941853 cites W2072656057 @default.
• W2023941853 cites W2073703410 @default.
• W2023941853 cites W2075964210 @default.
• W2023941853 cites W2077380876 @default.
• W2023941853 cites W2087668040 @default.
• W2023941853 cites W2094304122 @default.
• W2023941853 cites W2096412646 @default.
• W2023941853 cites W2107282719 @default.
• W2023941853 cites W2108971421 @default.
• W2023941853 cites W2114830943 @default.
• W2023941853 cites W2116453115 @default.
• W2023941853 cites W2119104917 @default.
• W2023941853 cites W2119241449 @default.
• W2023941853 cites W2126309541 @default.
• W2023941853 cites W2131587907 @default.
• W2023941853 cites W2138522501 @default.
• W2023941853 cites W2142984603 @default.
• W2023941853 cites W2143685761 @default.
• W2023941853 cites W2146997704 @default.
• W2023941853 cites W2151527887 @default.
• W2023941853 cites W2157907141 @default.
• W2023941853 cites W2159059102 @default.
• W2023941853 cites W2162811155 @default.
• W2023941853 cites W2163661774 @default.
• W2023941853 cites W2170605098 @default.
• W2023941853 cites W2171353065 @default.
• W2023941853 cites W2336372367 @default.
• W2023941853 cites W2341084977 @default.
• W2023941853 cites W2411079246 @default.
• W2023941853 cites W2470734866 @default.
• W2023941853 cites W2501988626 @default.
• W2023941853 cites W2503581259 @default.
• W2023941853 cites W2908712623 @default.
• W2023941853 cites W2909549806 @default.
• W2023941853 cites W2910084172 @default.
• W2023941853 cites W2910276023 @default.
• W2023941853 cites W2910781470 @default.
• W2023941853 cites W2910966882 @default.
• W2023941853 cites W2981864809 @default.
• W2023941853 cites W2981994584 @default.
• W2023941853 cites W2982286678 @default.
• W2023941853 cites W4250713120 @default.
• W2023941853 doi "https://doi.org/10.1130/b26325.1" @default.
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