FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2017001176> ?p ?o ?g. }

• W2017001176 endingPage "130" @default.
• W2017001176 startingPage "87" @default.
• W2017001176 abstract "The Thor-Odin dome is a large structural culmination along the eastern margin of the Shuswap terrain. Previous workers have presented divergent models for the origin of the dome. Some have proposed that it is a product of diapiric uprise of material from the lower crust; alternatively, the dome is interpreted to have formed from the interference of later folding. This study presents the results of a detailed analysis of new data on the structure, pattern of strain variation and metamorphic fabric of the dome. These data together with new geochronological and metamorphic phase assemblage information provide the basis for a revised interpretation of the evolution of the Thor-Odin gneiss dome. The pre-doming evolution of the Thor-Odin gneiss dome was characterized by the formation of large-scale nappe structures and the imbrication of Archean basement rocks with the Cambrian and younger cover rock sequence. The first period of deformation (Phase One) consisted of large-scale infolding of the cover rock sequence into the basement rocks. The Pingston fold in the core of the dome is a product of this event. The second period of deformation (Phase Two) was marked by the forcing of wedges of basement into the cores of northerly-directed nappes. These structures had no observable effect on the central core zone, which is here termed the Autochthonous Core Gneiss Domain. The third period of deformation (Phase Three) was co-axial with Phase Two and consisted of imbrication and refolding of the upper levels of the stack of Phase Two nappes. The actual domal shape was formed by fold interference of Phases Four, Five and Six, which were upright, chevron-style, flexural-slip folds with northwest, southwest and northerly-trending axial planes. The “doming” events occurred at upper crustal levels, probably during the Tertiary. Analysis of the strain pattern suggests that little of the total deformational strain is related to these dome-forming deformations. This outline of the events that formed the dome is consistent with the new geochronological results and interpretation of metamorphic phase assemblages. Cordierite-gedrite-sillimanite assemblages, previously interpreted as indicating 1000 MPa pressure, probably formed under reduced water fugacities and 500–700 MPa total pressure. The Thor-Odin gneiss dome thus provides no evidence for lower crustal upwelling related either to dome formation or to the formation of the Rocky Mountain thrust belt." @default.
• W2017001176 created "2016-06-24" @default.
• W2017001176 creator A5075352192 @default.
• W2017001176 date "1984-01-01" @default.
• W2017001176 modified "2023-09-26" @default.
• W2017001176 title "Structural evolution of the Thor-Odin gneiss dome" @default.
• W2017001176 cites W1964102003 @default.
• W2017001176 cites W1966427354 @default.
• W2017001176 cites W1968596577 @default.
• W2017001176 cites W1968639756 @default.
• W2017001176 cites W1970188264 @default.
• W2017001176 cites W1971522185 @default.
• W2017001176 cites W1974681337 @default.
• W2017001176 cites W1983426770 @default.
• W2017001176 cites W1989151361 @default.
• W2017001176 cites W1990731429 @default.
• W2017001176 cites W1995916598 @default.
• W2017001176 cites W2018095920 @default.
• W2017001176 cites W2018449519 @default.
• W2017001176 cites W2020731718 @default.
• W2017001176 cites W2022373295 @default.
• W2017001176 cites W2026302714 @default.
• W2017001176 cites W2029950481 @default.
• W2017001176 cites W2034787316 @default.
• W2017001176 cites W2036966699 @default.
• W2017001176 cites W2041716321 @default.
• W2017001176 cites W2055075733 @default.
• W2017001176 cites W2064560274 @default.
• W2017001176 cites W2066535772 @default.
• W2017001176 cites W2069162020 @default.
• W2017001176 cites W2089053123 @default.
• W2017001176 cites W2091097722 @default.
• W2017001176 cites W2091781102 @default.
• W2017001176 cites W2100445854 @default.
• W2017001176 cites W2125645755 @default.
• W2017001176 cites W2246972378 @default.
• W2017001176 cites W2317796819 @default.
• W2017001176 cites W2328089775 @default.
• W2017001176 doi "https://doi.org/10.1016/0040-1951(84)90044-1" @default.
• W2017001176 hasPublicationYear "1984" @default.
• W2017001176 type Work @default.
• W2017001176 sameAs 2017001176 @default.
• W2017001176 citedByCount "47" @default.
• W2017001176 countsByYear W20170011762012 @default.
• W2017001176 countsByYear W20170011762014 @default.
• W2017001176 countsByYear W20170011762016 @default.
• W2017001176 countsByYear W20170011762018 @default.
• W2017001176 countsByYear W20170011762019 @default.
• W2017001176 countsByYear W20170011762020 @default.
• W2017001176 countsByYear W20170011762021 @default.
• W2017001176 countsByYear W20170011762022 @default.
• W2017001176 countsByYear W20170011762023 @default.
• W2017001176 crossrefType "journal-article" @default.
• W2017001176 hasAuthorship W2017001176A5075352192 @default.
• W2017001176 hasConcept C114793014 @default.
• W2017001176 hasConcept C127313418 @default.
• W2017001176 hasConcept C127413603 @default.
• W2017001176 hasConcept C136137745 @default.
• W2017001176 hasConcept C147176958 @default.
• W2017001176 hasConcept C149347711 @default.
• W2017001176 hasConcept C153220577 @default.
• W2017001176 hasConcept C165205528 @default.
• W2017001176 hasConcept C171701179 @default.
• W2017001176 hasConcept C17409809 @default.
• W2017001176 hasConcept C189092281 @default.
• W2017001176 hasConcept C199007388 @default.
• W2017001176 hasConcept C26687426 @default.
• W2017001176 hasConcept C2776698055 @default.
• W2017001176 hasConcept C2780802278 @default.
• W2017001176 hasConcept C2781297371 @default.
• W2017001176 hasConcept C5900021 @default.
• W2017001176 hasConcept C63014310 @default.
• W2017001176 hasConcept C77928131 @default.
• W2017001176 hasConceptScore W2017001176C114793014 @default.
• W2017001176 hasConceptScore W2017001176C127313418 @default.
• W2017001176 hasConceptScore W2017001176C127413603 @default.
• W2017001176 hasConceptScore W2017001176C136137745 @default.
• W2017001176 hasConceptScore W2017001176C147176958 @default.
• W2017001176 hasConceptScore W2017001176C149347711 @default.
• W2017001176 hasConceptScore W2017001176C153220577 @default.
• W2017001176 hasConceptScore W2017001176C165205528 @default.
• W2017001176 hasConceptScore W2017001176C171701179 @default.
• W2017001176 hasConceptScore W2017001176C17409809 @default.
• W2017001176 hasConceptScore W2017001176C189092281 @default.
• W2017001176 hasConceptScore W2017001176C199007388 @default.
• W2017001176 hasConceptScore W2017001176C26687426 @default.
• W2017001176 hasConceptScore W2017001176C2776698055 @default.
• W2017001176 hasConceptScore W2017001176C2780802278 @default.
• W2017001176 hasConceptScore W2017001176C2781297371 @default.
• W2017001176 hasConceptScore W2017001176C5900021 @default.
• W2017001176 hasConceptScore W2017001176C63014310 @default.
• W2017001176 hasConceptScore W2017001176C77928131 @default.
• W2017001176 hasIssue "1-2" @default.
• W2017001176 hasLocation W20170011761 @default.
• W2017001176 hasOpenAccess W2017001176 @default.
• W2017001176 hasPrimaryLocation W20170011761 @default.
• W2017001176 hasRelatedWork W1142018654 @default.
• W2017001176 hasRelatedWork W1966373346 @default.

• next