FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2103116164> ?p ?o ?g. }

• W2103116164 endingPage "173" @default.
• W2103116164 startingPage "162" @default.
• W2103116164 abstract "Metamorphic core complexes represent concentrated zones of crustal extension; universally, the hanging walls of these systems are extensively fractured, attesting to the significant horizontal extension above the evolving detachment zone. Recent analysis of a large grid of 2-D seismic reflection lines within the Tucson Basin of southeastern Arizona has facilitated a nearly three-dimensional interpretation of subsurface features related to Cenozoic crustal extension. Within the northern Tucson Basin, the Catalina detachment fault dips 23–35° to the southwest from the western flank of the Catalina/Rincon Metamorphic Core Complex. In the southern portion of the basin, the NE-trending Santa Rita normal fault dips 15–20° to the northwest from the western flank of the Santa Rita Mountains and is cut by the Catalina detachment beneath the central Tucson Basin. The orientation of the Santa Rita fault is problematical in that its orientation is nearly perpendicular to extension directions in the region, while geologic and seismic reflection evidence indicates that the Catalina detachment and Santa Rita fault were active synchronously. One possible explanation is that the Santa Rita fault is accommodating along-strike upper-plate deformation in response to core complex emplacement. To test this, we employed a finite-element modeling approach. A two-dimensional model consisting of a homogenous elastic material undergoing uniform extension is used to study changes in stresses and displacements in proximity to a zone of weakness representing a detachment fault in the upper crust. Away from the detachment fault, primary principal stresses are oriented parallel to the regional extension direction as expected. Near the detachment, extension in the system produces a rotation of the primary principal stresses of nearly 60° with respect to the regional stress field around the end of the fault. Additionally, the model predicts mechanical failure of the upper-plate of the detachment system to the south of the Catalina core complex. This model supports our interpretation that the orientation and early displacement noted on the Santa Rita fault is the result of a perturbation in the regional stress field caused by the Catalina detachment and the associated brittle failure of the upper-plate from the extreme crustal extension associated with core complex emplacement." @default.
• W2103116164 created "2016-06-24" @default.
• W2103116164 creator A5014356134 @default.
• W2103116164 creator A5051877419 @default.
• W2103116164 date "2010-06-01" @default.
• W2103116164 modified "2023-09-26" @default.
• W2103116164 title "Along-strike upper-plate deformation in response to metamorphic core complex emplacement, SE Arizona" @default.
• W2103116164 cites W1975633233 @default.
• W2103116164 cites W1979739422 @default.
• W2103116164 cites W1982909722 @default.
• W2103116164 cites W1984706520 @default.
• W2103116164 cites W1994323983 @default.
• W2103116164 cites W1995115331 @default.
• W2103116164 cites W2010675804 @default.
• W2103116164 cites W2027937448 @default.
• W2103116164 cites W2038989614 @default.
• W2103116164 cites W2048553158 @default.
• W2103116164 cites W2058834991 @default.
• W2103116164 cites W2060888950 @default.
• W2103116164 cites W2066860843 @default.
• W2103116164 cites W2086964222 @default.
• W2103116164 cites W2087372055 @default.
• W2103116164 cites W2116453115 @default.
• W2103116164 cites W2124474119 @default.
• W2103116164 cites W2128162245 @default.
• W2103116164 cites W2138655928 @default.
• W2103116164 cites W2146442976 @default.
• W2103116164 cites W2146671435 @default.
• W2103116164 cites W2170853836 @default.
• W2103116164 cites W2402344186 @default.
• W2103116164 cites W2418430299 @default.
• W2103116164 doi "https://doi.org/10.1016/j.tecto.2009.07.017" @default.
• W2103116164 hasPublicationYear "2010" @default.
• W2103116164 type Work @default.
• W2103116164 sameAs 2103116164 @default.
• W2103116164 citedByCount "3" @default.
• W2103116164 countsByYear W21031161642019 @default.
• W2103116164 countsByYear W21031161642020 @default.
• W2103116164 countsByYear W21031161642022 @default.
• W2103116164 crossrefType "journal-article" @default.
• W2103116164 hasAuthorship W2103116164A5014356134 @default.
• W2103116164 hasAuthorship W2103116164A5051877419 @default.
• W2103116164 hasConcept C109007969 @default.
• W2103116164 hasConcept C127313418 @default.
• W2103116164 hasConcept C136137745 @default.
• W2103116164 hasConcept C144024400 @default.
• W2103116164 hasConcept C151730666 @default.
• W2103116164 hasConcept C155627805 @default.
• W2103116164 hasConcept C165205528 @default.
• W2103116164 hasConcept C175551986 @default.
• W2103116164 hasConcept C185339796 @default.
• W2103116164 hasConcept C19165224 @default.
• W2103116164 hasConcept C26687426 @default.
• W2103116164 hasConcept C2776698055 @default.
• W2103116164 hasConcept C2780395675 @default.
• W2103116164 hasConcept C63014310 @default.
• W2103116164 hasConcept C73707237 @default.
• W2103116164 hasConcept C77928131 @default.
• W2103116164 hasConceptScore W2103116164C109007969 @default.
• W2103116164 hasConceptScore W2103116164C127313418 @default.
• W2103116164 hasConceptScore W2103116164C136137745 @default.
• W2103116164 hasConceptScore W2103116164C144024400 @default.
• W2103116164 hasConceptScore W2103116164C151730666 @default.
• W2103116164 hasConceptScore W2103116164C155627805 @default.
• W2103116164 hasConceptScore W2103116164C165205528 @default.
• W2103116164 hasConceptScore W2103116164C175551986 @default.
• W2103116164 hasConceptScore W2103116164C185339796 @default.
• W2103116164 hasConceptScore W2103116164C19165224 @default.
• W2103116164 hasConceptScore W2103116164C26687426 @default.
• W2103116164 hasConceptScore W2103116164C2776698055 @default.
• W2103116164 hasConceptScore W2103116164C2780395675 @default.
• W2103116164 hasConceptScore W2103116164C63014310 @default.
• W2103116164 hasConceptScore W2103116164C73707237 @default.
• W2103116164 hasConceptScore W2103116164C77928131 @default.
• W2103116164 hasIssue "1-4" @default.
• W2103116164 hasLocation W21031161641 @default.
• W2103116164 hasOpenAccess W2103116164 @default.
• W2103116164 hasPrimaryLocation W21031161641 @default.
• W2103116164 hasRelatedWork W2038989614 @default.
• W2103116164 hasRelatedWork W2076289454 @default.
• W2103116164 hasRelatedWork W2164643951 @default.
• W2103116164 hasRelatedWork W2352760114 @default.
• W2103116164 hasRelatedWork W2527157123 @default.
• W2103116164 hasRelatedWork W2566014292 @default.
• W2103116164 hasRelatedWork W2596905136 @default.
• W2103116164 hasRelatedWork W4297221196 @default.
• W2103116164 hasRelatedWork W4384927870 @default.
• W2103116164 hasRelatedWork W1672251905 @default.
• W2103116164 hasVolume "488" @default.
• W2103116164 isParatext "false" @default.
• W2103116164 isRetracted "false" @default.
• W2103116164 magId "2103116164" @default.
• W2103116164 workType "article" @default.