FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1536700970> ?p ?o ?g. }

• W1536700970 abstract "Shear‐wave splitting observations in the region of the upper mantle enveloping subduction zones have been interpreted as showing extensive regions of trench‐parallel flow, despite the difficulty of reconciling such behavior with a sound model based on the forces that drive mantle motion. To gain insight into the observations, we systematically investigate flow patterns around the cold downwelling sheets associated with consumed plate material in a three‐dimensional numerical mantle convection model. First, we compare results from calculations employing prescribed plate geometries and kinematic plate velocities where the convergent plate boundary morphology is varied while keeping the plate velocity and convective parameters fixed. Subsequently, we examine the flow around sheet‐like downwellings in a number of convection calculations featuring dynamically evolving plate velocities. All of the calculations include thick viscous plates and a stratified mantle viscosity. In all of the models examined, we find that at mid‐upper mantle depths, flow directions no longer align with plate motion and the influence of buoyancy‐driven downwellings clearly dominates flow solutions. In the first models analyzed, a pair of plates are included in the calculations, and the large‐scale flow is generally roll‐like. In the final model we investigate the interaction of four plates and a plate geometry characterized by triple junctions. We examine a sequence from this calculation that features a triple junction of convergent boundaries. In this model, large‐scale flow characterized by convection rolls is superseded by a complex flow solution where flow in the mid‐upper mantle neither aligns uniformly with the plate motion nor necessarily follows the forcing associated with local buoyancy sources. In this setting, upper mantle flow in the vicinity of the sheet‐like downwellings featured in the solution moves orthogonal, obliquely, and even parallel to different sections of the convergent plate boundaries. In the latter case our calculations of the deformation of a fixed volume parcel of upper mantle material suggest that an olivine lattice‐preferred orientation should develop that would result in a fast polarizing direction for seismic shear waves parallel to the slab. Our findings have implications for the interpretation of flow in the upper mantle based on seismic anisotropy." @default.
• W1536700970 created "2016-06-24" @default.
• W1536700970 creator A5052103732 @default.
• W1536700970 creator A5068508635 @default.
• W1536700970 creator A5083083922 @default.
• W1536700970 creator A5086300371 @default.
• W1536700970 date "2007-08-01" @default.
• W1536700970 modified "2023-10-13" @default.
• W1536700970 title "Influence of convergent plate boundaries on upper mantle flow and implications for seismic anisotropy" @default.
• W1536700970 cites W1493714271 @default.
• W1536700970 cites W1552909705 @default.
• W1536700970 cites W1601648958 @default.
• W1536700970 cites W1608015442 @default.
• W1536700970 cites W1967202511 @default.
• W1536700970 cites W1969409033 @default.
• W1536700970 cites W1975324737 @default.
• W1536700970 cites W1981224522 @default.
• W1536700970 cites W1987006553 @default.
• W1536700970 cites W1987153889 @default.
• W1536700970 cites W1995988653 @default.
• W1536700970 cites W1996660735 @default.
• W1536700970 cites W2000766983 @default.
• W1536700970 cites W2007827400 @default.
• W1536700970 cites W2008526841 @default.
• W1536700970 cites W2009824639 @default.
• W1536700970 cites W2010631652 @default.
• W1536700970 cites W2013360601 @default.
• W1536700970 cites W2013536358 @default.
• W1536700970 cites W2021065582 @default.
• W1536700970 cites W2029570023 @default.
• W1536700970 cites W2031084439 @default.
• W1536700970 cites W2031556217 @default.
• W1536700970 cites W2032410808 @default.
• W1536700970 cites W2035104872 @default.
• W1536700970 cites W2035501773 @default.
• W1536700970 cites W2038193194 @default.
• W1536700970 cites W2038669248 @default.
• W1536700970 cites W2045115538 @default.
• W1536700970 cites W2046733489 @default.
• W1536700970 cites W2053398580 @default.
• W1536700970 cites W2053863496 @default.
• W1536700970 cites W2058368767 @default.
• W1536700970 cites W2062018184 @default.
• W1536700970 cites W2063287321 @default.
• W1536700970 cites W2067772844 @default.
• W1536700970 cites W2075101142 @default.
• W1536700970 cites W2080128098 @default.
• W1536700970 cites W2085283805 @default.
• W1536700970 cites W2097914838 @default.
• W1536700970 cites W2103311221 @default.
• W1536700970 cites W2106812239 @default.
• W1536700970 cites W2113925928 @default.
• W1536700970 cites W2116910913 @default.
• W1536700970 cites W2117074282 @default.
• W1536700970 cites W2117264814 @default.
• W1536700970 cites W2125510193 @default.
• W1536700970 cites W2125820637 @default.
• W1536700970 cites W2155223823 @default.
• W1536700970 cites W2161559349 @default.
• W1536700970 cites W2161590027 @default.
• W1536700970 cites W2162847319 @default.
• W1536700970 cites W2166106490 @default.
• W1536700970 cites W2167431014 @default.
• W1536700970 cites W2168934780 @default.
• W1536700970 cites W2482444110 @default.
• W1536700970 doi "https://doi.org/10.1029/2007gc001627" @default.
• W1536700970 hasPublicationYear "2007" @default.
• W1536700970 type Work @default.
• W1536700970 sameAs 1536700970 @default.
• W1536700970 citedByCount "20" @default.
• W1536700970 countsByYear W15367009702012 @default.
• W1536700970 countsByYear W15367009702013 @default.
• W1536700970 countsByYear W15367009702014 @default.
• W1536700970 countsByYear W15367009702017 @default.
• W1536700970 countsByYear W15367009702018 @default.
• W1536700970 crossrefType "journal-article" @default.
• W1536700970 hasAuthorship W1536700970A5052103732 @default.
• W1536700970 hasAuthorship W1536700970A5068508635 @default.
• W1536700970 hasAuthorship W1536700970A5083083922 @default.
• W1536700970 hasAuthorship W1536700970A5086300371 @default.
• W1536700970 hasBestOaLocation W15367009701 @default.
• W1536700970 hasConcept C10899652 @default.
• W1536700970 hasConcept C111368507 @default.
• W1536700970 hasConcept C119477230 @default.
• W1536700970 hasConcept C119601563 @default.
• W1536700970 hasConcept C121332964 @default.
• W1536700970 hasConcept C127313418 @default.
• W1536700970 hasConcept C146481406 @default.
• W1536700970 hasConcept C149348798 @default.
• W1536700970 hasConcept C154200439 @default.
• W1536700970 hasConcept C165205528 @default.
• W1536700970 hasConcept C190799397 @default.
• W1536700970 hasConcept C538625479 @default.
• W1536700970 hasConcept C57879066 @default.
• W1536700970 hasConcept C58097730 @default.
• W1536700970 hasConcept C64174561 @default.
• W1536700970 hasConcept C67236022 @default.
• W1536700970 hasConcept C73462661 @default.
• W1536700970 hasConcept C77928131 @default.
• W1536700970 hasConcept C8058405 @default.

• next