Matches in SemOpenAlex for { <https://semopenalex.org/work/W2040457939> ?p ?o ?g. }
Showing items 1 to 75 of
75
with 100 items per page.
- W2040457939 endingPage "251" @default.
- W2040457939 startingPage "225" @default.
- W2040457939 abstract "The propagation of a fault zone through homogeneous and layered sedimentary materials above a basement deflection was simulated using a finite-element solution for slow, incompressible viscous flow. The layered models represented a generalized stratigraphic section of the Paleozoic and Mesozoic strata of the Wyoming Province, U.S.A. Fractured elements within the models were determined for each increment of deformation using the Mohr-Coulomb fracture criterion and the viscosity of those elements was decreased prior to subsequent increments. In this manner the effects of local fracturing on subsequent deformation were included. In homogeneous models, failure begins near the basement deflection and propagates discontinuously upward. The length of the fault zone depends on the vertical velocity imposed on the bottom boundary and the width of the deflection. The resulting fault zone is a high-angle, rather straight, reverse fault which is in contrast to the curved, concave downward faults predicted by previous elastic analytical solutions. However, the analytical solutions were based on the initial stress field and do not take into consideration any changes that occur within the body during deformation. In contrast to this, the finite-element models can be used to study the changes in the state of a body that occur during deformation. Deformation rates determine the style of deformation and the location and intensity of fracturing. High gradients of mean pressure occur near the basement deflection and the fault zone is initiated in a region of anomalously low pressure produced by deformation. Faults develop as a consequence of the coalescense of fractured elements that occur during deformation. The width of the fault zone varied from layer to layer depending on its stiffness. Narrow fault zones develop in weak layers and wide zones in stiffer layers. In both homogeneous and layered models, extensional fractures occur near the surface on the upper block." @default.
- W2040457939 created "2016-06-24" @default.
- W2040457939 creator A5021441725 @default.
- W2040457939 creator A5031176945 @default.
- W2040457939 date "1980-06-01" @default.
- W2040457939 modified "2023-09-27" @default.
- W2040457939 title "Viscosity-based numerical model for fault-zone development in drape folding" @default.
- W2040457939 cites W112547364 @default.
- W2040457939 cites W1485790192 @default.
- W2040457939 cites W1993522146 @default.
- W2040457939 cites W2001566429 @default.
- W2040457939 cites W2010339634 @default.
- W2040457939 cites W2035461734 @default.
- W2040457939 cites W2042820448 @default.
- W2040457939 cites W2043033721 @default.
- W2040457939 cites W2058243810 @default.
- W2040457939 cites W2119560598 @default.
- W2040457939 cites W2127528680 @default.
- W2040457939 cites W2133228730 @default.
- W2040457939 cites W2137194533 @default.
- W2040457939 cites W2138183756 @default.
- W2040457939 cites W2343166190 @default.
- W2040457939 doi "https://doi.org/10.1016/0040-1951(80)90048-7" @default.
- W2040457939 hasPublicationYear "1980" @default.
- W2040457939 type Work @default.
- W2040457939 sameAs 2040457939 @default.
- W2040457939 citedByCount "6" @default.
- W2040457939 crossrefType "journal-article" @default.
- W2040457939 hasAuthorship W2040457939A5021441725 @default.
- W2040457939 hasAuthorship W2040457939A5031176945 @default.
- W2040457939 hasConcept C111368507 @default.
- W2040457939 hasConcept C120665830 @default.
- W2040457939 hasConcept C121332964 @default.
- W2040457939 hasConcept C127313418 @default.
- W2040457939 hasConcept C135628077 @default.
- W2040457939 hasConcept C204366326 @default.
- W2040457939 hasConcept C2524010 @default.
- W2040457939 hasConcept C2781355719 @default.
- W2040457939 hasConcept C3161131 @default.
- W2040457939 hasConcept C33923547 @default.
- W2040457939 hasConcept C57879066 @default.
- W2040457939 hasConcept C97355855 @default.
- W2040457939 hasConceptScore W2040457939C111368507 @default.
- W2040457939 hasConceptScore W2040457939C120665830 @default.
- W2040457939 hasConceptScore W2040457939C121332964 @default.
- W2040457939 hasConceptScore W2040457939C127313418 @default.
- W2040457939 hasConceptScore W2040457939C135628077 @default.
- W2040457939 hasConceptScore W2040457939C204366326 @default.
- W2040457939 hasConceptScore W2040457939C2524010 @default.
- W2040457939 hasConceptScore W2040457939C2781355719 @default.
- W2040457939 hasConceptScore W2040457939C3161131 @default.
- W2040457939 hasConceptScore W2040457939C33923547 @default.
- W2040457939 hasConceptScore W2040457939C57879066 @default.
- W2040457939 hasConceptScore W2040457939C97355855 @default.
- W2040457939 hasIssue "1-3" @default.
- W2040457939 hasLocation W20404579391 @default.
- W2040457939 hasOpenAccess W2040457939 @default.
- W2040457939 hasPrimaryLocation W20404579391 @default.
- W2040457939 hasRelatedWork W204793539 @default.
- W2040457939 hasRelatedWork W2119348969 @default.
- W2040457939 hasRelatedWork W2138870000 @default.
- W2040457939 hasRelatedWork W2256606375 @default.
- W2040457939 hasRelatedWork W2379224710 @default.
- W2040457939 hasRelatedWork W2400153779 @default.
- W2040457939 hasRelatedWork W2667301796 @default.
- W2040457939 hasRelatedWork W3028013418 @default.
- W2040457939 hasRelatedWork W3045482405 @default.
- W2040457939 hasRelatedWork W3178185328 @default.
- W2040457939 hasVolume "66" @default.
- W2040457939 isParatext "false" @default.
- W2040457939 isRetracted "false" @default.
- W2040457939 magId "2040457939" @default.
- W2040457939 workType "article" @default.