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• W1978494313 abstract "Research Article| February 01, 1987 Tectonic denudation of the Shuswap metamorphic terrane of southeastern British Columbia Richard L. Brown; Richard L. Brown 1Ottawa-Carleton Centre for Geoscience Studies and Carleton University, Ottawa, Ontario K1S 5B6, Canada Search for other works by this author on: GSW Google Scholar J. Murray J. Murray 2Department of Geology, Middlebury College Middlebury, Vermont 05753 Search for other works by this author on: GSW Google Scholar Author and Article Information Richard L. Brown 1Ottawa-Carleton Centre for Geoscience Studies and Carleton University, Ottawa, Ontario K1S 5B6, Canada J. Murray 2Department of Geology, Middlebury College Middlebury, Vermont 05753 Publisher: Geological Society of America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1987) 15 (2): 142–146. https://doi.org/10.1130/0091-7613(1987)15<142:TDOTSM>2.0.CO;2 Article history First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Richard L. Brown, J. Murray; Tectonic denudation of the Shuswap metamorphic terrane of southeastern British Columbia. Geology 1987;; 15 (2): 142–146. doi: https://doi.org/10.1130/0091-7613(1987)15<142:TDOTSM>2.0.CO;2 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 Large-scale over-thrusting and regional extension are both known to have been operative within the Shuswap metamorphic terrane of the southern Omineca belt. The Monashee core complex of the northern Shuswap terrane is interpreted to be a crustal-scale duplex that was developed during late Mesozoic shortening and thickening of the crust. Uplift of the Monashee complex, caused by basement duplexing, is estimated to have been in excess of 25 km. Late Cretaceous overthrusting of high-grade metamorphic and related plutonic rocks, during later stages of uplift and basement duplexing, led to weakening of the crust and to gravitationally driven extension of a regional crustal welt (Shuswap culmination). Denudation and spreading of this uplifted metamorphic terrane are attributed to displacements across listric-normal shear zones and faults localized along the outward-dipping flanks of the Shuswap culmination. Total extension across the Shuswap culmination at the northern end of the Monashee complex is estimated to be no greater than 30%. This model of denudation and gravity-induced spreading is extrapolated southward into the Valhalla and Okanagan regions, where extension may be far more significant. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal 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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• W1978494313 title "Tectonic denudation of the Shuswap metamorphic terrane of southeastern British Columbia" @default.
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