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Magmatic evolution of the eastern Coast plutonic complex, Bella Coola region, west-central British Columbia

J. Brian Mahoney, Sarah M. Gordee, James W. Haggart, Richard M. Friedman, Larry J. Diakow and Glenn J. Woodsworth
Magmatic evolution of the eastern Coast plutonic complex, Bella Coola region, west-central British Columbia
Geological Society of America Bulletin (September 2009) 121 (9-10): 1362-1380

Abstract

The eastern Coast Plutonic Complex in west-central British Columbia (51-54 degrees 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.


ISSN: 0016-7606
EISSN: 1943-2674
Coden: BUGMAF
Serial Title: Geological Society of America Bulletin
Serial Volume: 121
Serial Issue: 9-10
Title: Magmatic evolution of the eastern Coast plutonic complex, Bella Coola region, west-central British Columbia
Affiliation: University of Wisconsin-Eau Claire, Department of Geology, Eau Claire, WI, United States
Pages: 1362-1380
Published: 200909
Text Language: English
Publisher: Geological Society of America (GSA), Boulder, CO, United States
References: 101
Accession Number: 2009-074686
Categories: Igneous and metamorphic petrology
Document Type: Serial
Bibliographic Level: Analytic
Annotation: With GSA Data Repository Item 2009075
Illustration Description: illus. incl. 3 tables, geol. sketch maps
N51°45'00" - N54°00'00", W128°00'00" - W126°00'00"
Secondary Affiliation: Geological Survey of Canada, CAN, CanadaUniversity of British Columbia, CAN, CanadaBritish Columbia Ministry of Energy and Mines, CAN, Canada
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2019, American Geosciences Institute. Reference includes data from GeoScienceWorld, Alexandria, VA, United States. Reference includes data supplied by the Geological Society of America, Boulder, CO, United States
Update Code: 200940
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