FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2372015504> ?p ?o ?g. }

• W2372015504 abstract "We study a simple model of the deformation caused by the collision between two continental plates,in which the continental collision is simplified as the collision between two viscoelastic plates.A discontinuous deformation interface is chosen to approximate the fracture zone between the two continental plates.A finite element approach—three dimensional viscoelastic Lagrangian discontinuous deformation analysis(LDDA) is used to study the role of the discontinuous deformation interface on the collisional deformation between two viscoelastic plates.Based on this,we investigate the influence of the dip angle and friction factor of a collision-related fracture zone on the deformation caused by the collision between two continents.The results show some remarkable characteristics.Although the model's geometric size and boundary conditions are patterned after the India-Asia collision,the outcome may be applicable to more general situations.The results show that whether the dip angle or friction factor of the fracture zone does have an important effect on the continental collision deformation.With a dip angle between 15° and 30°,the uplift of an obducted plate during continental collision is much higher,and able to form a high mountain.The uplift is greatest with a dip angle of 15°;whereas with a dip angle between 30° and 45°,the subduction depth of a plate is much deeper,and able to form a deep basin.The subduction depth is greatest with a dip angle of 45°.When the dip angle is equal to or greater than 75°,subduction and obduction movements between two continents become undistinguishable.On the other hand,the less the friction factor of a collision-related fracture zone,the stronger the subduction and obduction movements between two continents,and the friction factor should not be larger than 0.2 so as to be able to form a high mountain and a deep basin by the collision between two continents.The general feature of deformation caused by the collision between two continents also reveals that,during the collision process,apart from a foreland basin and high mountains being formed,there is another compressive depression with an asymmetric structure developed on the side of the obducted plate,which is much easier to be formed when the dip angle of the collisional fracture zone is between 15° and 30° and is the deepest with a dip angle of 30°.This implies that the compressive depression is controlled by both subduction and obduction between two continents." @default.
• W2372015504 created "2016-06-24" @default.
• W2372015504 creator A5004513442 @default.
• W2372015504 creator A5010088857 @default.
• W2372015504 creator A5044440131 @default.
• W2372015504 creator A5073480923 @default.
• W2372015504 date "2006-01-01" @default.
• W2372015504 modified "2023-09-27" @default.
• W2372015504 title "The effects of the dip angle and friction factor of a collision-related fracture zone on the deformation caused by the collision between two continental plates." @default.
• W2372015504 hasPublicationYear "2006" @default.
• W2372015504 type Work @default.
• W2372015504 sameAs 2372015504 @default.
• W2372015504 citedByCount "0" @default.
• W2372015504 crossrefType "journal-article" @default.
• W2372015504 hasAuthorship W2372015504A5004513442 @default.
• W2372015504 hasAuthorship W2372015504A5010088857 @default.
• W2372015504 hasAuthorship W2372015504A5044440131 @default.
• W2372015504 hasAuthorship W2372015504A5073480923 @default.
• W2372015504 hasConcept C111368507 @default.
• W2372015504 hasConcept C121704057 @default.
• W2372015504 hasConcept C127313418 @default.
• W2372015504 hasConcept C154200439 @default.
• W2372015504 hasConcept C165205528 @default.
• W2372015504 hasConcept C187320778 @default.
• W2372015504 hasConcept C192367031 @default.
• W2372015504 hasConcept C192717286 @default.
• W2372015504 hasConcept C204366326 @default.
• W2372015504 hasConcept C2524010 @default.
• W2372015504 hasConcept C33923547 @default.
• W2372015504 hasConcept C38652104 @default.
• W2372015504 hasConcept C41008148 @default.
• W2372015504 hasConcept C43369102 @default.
• W2372015504 hasConcept C58097730 @default.
• W2372015504 hasConcept C60365795 @default.
• W2372015504 hasConcept C75643213 @default.
• W2372015504 hasConcept C77928131 @default.
• W2372015504 hasConcept C8058405 @default.
• W2372015504 hasConceptScore W2372015504C111368507 @default.
• W2372015504 hasConceptScore W2372015504C121704057 @default.
• W2372015504 hasConceptScore W2372015504C127313418 @default.
• W2372015504 hasConceptScore W2372015504C154200439 @default.
• W2372015504 hasConceptScore W2372015504C165205528 @default.
• W2372015504 hasConceptScore W2372015504C187320778 @default.
• W2372015504 hasConceptScore W2372015504C192367031 @default.
• W2372015504 hasConceptScore W2372015504C192717286 @default.
• W2372015504 hasConceptScore W2372015504C204366326 @default.
• W2372015504 hasConceptScore W2372015504C2524010 @default.
• W2372015504 hasConceptScore W2372015504C33923547 @default.
• W2372015504 hasConceptScore W2372015504C38652104 @default.
• W2372015504 hasConceptScore W2372015504C41008148 @default.
• W2372015504 hasConceptScore W2372015504C43369102 @default.
• W2372015504 hasConceptScore W2372015504C58097730 @default.
• W2372015504 hasConceptScore W2372015504C60365795 @default.
• W2372015504 hasConceptScore W2372015504C75643213 @default.
• W2372015504 hasConceptScore W2372015504C77928131 @default.
• W2372015504 hasConceptScore W2372015504C8058405 @default.
• W2372015504 hasLocation W23720155041 @default.
• W2372015504 hasOpenAccess W2372015504 @default.
• W2372015504 hasPrimaryLocation W23720155041 @default.
• W2372015504 hasRelatedWork W103553079 @default.
• W2372015504 hasRelatedWork W106339988 @default.
• W2372015504 hasRelatedWork W13831553 @default.
• W2372015504 hasRelatedWork W1590212289 @default.
• W2372015504 hasRelatedWork W1641307010 @default.
• W2372015504 hasRelatedWork W1968948374 @default.
• W2372015504 hasRelatedWork W1997764668 @default.
• W2372015504 hasRelatedWork W2035781233 @default.
• W2372015504 hasRelatedWork W2132537895 @default.
• W2372015504 hasRelatedWork W2186490078 @default.
• W2372015504 hasRelatedWork W2189157363 @default.
• W2372015504 hasRelatedWork W2313203793 @default.
• W2372015504 hasRelatedWork W2626112459 @default.
• W2372015504 hasRelatedWork W2743546302 @default.
• W2372015504 hasRelatedWork W2786637963 @default.
• W2372015504 hasRelatedWork W2894839895 @default.
• W2372015504 hasRelatedWork W2961724387 @default.
• W2372015504 hasRelatedWork W2978322491 @default.
• W2372015504 hasRelatedWork W3007174238 @default.
• W2372015504 hasRelatedWork W19552917 @default.
• W2372015504 isParatext "false" @default.
• W2372015504 isRetracted "false" @default.
• W2372015504 magId "2372015504" @default.
• W2372015504 workType "article" @default.