FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2022972464> ?p ?o ?g. }

• W2022972464 endingPage "2394" @default.
• W2022972464 startingPage "2391" @default.
• W2022972464 abstract "The morphology of the Rivera plate subducted beneath the Jalisco block in western Mexico is determined from accurately located hypocenters of locally recorded microearthquakes, and from earthquakes with magnitude mb≥4.5 recorded at teleseismic distances. The hypocenters of these latter earthquakes are relocated, and for five of them the focal depth is constrained by the inversion of long-period body waves. The Wadati-Benioff zone inferred from these data indicates a steep subduction of the Rivera plate that resembles the geometry of subduction of the Cocos plate beneath Central America. It is, however, very different from the shallower and almost subhorizontal subduction of the Cocos plate observed in southern Mexico, southeast of this region. The Rivera plate is comparable to the Juan de Fuca plate in terms of the small areal extent, young seafloor age, low relative velocity, and low teleseismic activity in the subduction zone. This study shows that the dip of both the Juan de Fuca and Rivera plates are similar once they are decoupled from the overriding continental crust. The downgoing Rivera plate initially starts with a dip of ∼10° down to a depth of 20 km and then increases gradually to a constant dip of ∼50° below a depth of 40 km. Intermediate-depth seismicity is low in this zone associated with the subduction of the slow (2 cm/yr) and young (9 m.y.) Rivera plate. The maximum depth extent of earthquakes observed in the Rivera subduction zone is about 130 km. The andesitic, calc-alkaline Colima volcano appears to be directly related to the subduction of the Rivera plate. To the NW of this volcano, the observed Quaternary volcanism in the Jalisco block, which is parallel to the trench, may also be explained by the subduction of the Rivera plate." @default.
• W2022972464 created "2016-06-24" @default.
• W2022972464 creator A5042535907 @default.
• W2022972464 creator A5046314018 @default.
• W2022972464 date "1993-11-05" @default.
• W2022972464 modified "2023-09-24" @default.
• W2022972464 title "Steep subduction geometry of the Rivera Plate beneath the Jalisco Block in western Mexico" @default.
• W2022972464 cites W1514799976 @default.
• W2022972464 cites W1967331152 @default.
• W2022972464 cites W1969296108 @default.
• W2022972464 cites W1982112423 @default.
• W2022972464 cites W1983275123 @default.
• W2022972464 cites W2002077405 @default.
• W2022972464 cites W2039802692 @default.
• W2022972464 cites W2061847045 @default.
• W2022972464 cites W2063018988 @default.
• W2022972464 cites W2104052878 @default.
• W2022972464 cites W2104449480 @default.
• W2022972464 cites W2119679773 @default.
• W2022972464 cites W2138639675 @default.
• W2022972464 cites W2154869178 @default.
• W2022972464 cites W2548530909 @default.
• W2022972464 doi "https://doi.org/10.1029/93gl02794" @default.
• W2022972464 hasPublicationYear "1993" @default.
• W2022972464 type Work @default.
• W2022972464 sameAs 2022972464 @default.
• W2022972464 citedByCount "110" @default.
• W2022972464 countsByYear W20229724642013 @default.
• W2022972464 countsByYear W20229724642014 @default.
• W2022972464 countsByYear W20229724642015 @default.
• W2022972464 countsByYear W20229724642016 @default.
• W2022972464 countsByYear W20229724642017 @default.
• W2022972464 countsByYear W20229724642018 @default.
• W2022972464 countsByYear W20229724642019 @default.
• W2022972464 countsByYear W20229724642020 @default.
• W2022972464 countsByYear W20229724642021 @default.
• W2022972464 countsByYear W20229724642022 @default.
• W2022972464 countsByYear W20229724642023 @default.
• W2022972464 crossrefType "journal-article" @default.
• W2022972464 hasAuthorship W2022972464A5042535907 @default.
• W2022972464 hasAuthorship W2022972464A5046314018 @default.
• W2022972464 hasConcept C117485682 @default.
• W2022972464 hasConcept C119477230 @default.
• W2022972464 hasConcept C120806208 @default.
• W2022972464 hasConcept C127313418 @default.
• W2022972464 hasConcept C141646446 @default.
• W2022972464 hasConcept C154200439 @default.
• W2022972464 hasConcept C165205528 @default.
• W2022972464 hasConcept C192241223 @default.
• W2022972464 hasConcept C2524010 @default.
• W2022972464 hasConcept C2776698055 @default.
• W2022972464 hasConcept C2777210771 @default.
• W2022972464 hasConcept C2778261408 @default.
• W2022972464 hasConcept C33923547 @default.
• W2022972464 hasConcept C36986328 @default.
• W2022972464 hasConcept C58097730 @default.
• W2022972464 hasConcept C64174561 @default.
• W2022972464 hasConcept C77928131 @default.
• W2022972464 hasConcept C8058405 @default.
• W2022972464 hasConcept C83176761 @default.
• W2022972464 hasConcept C90523207 @default.
• W2022972464 hasConceptScore W2022972464C117485682 @default.
• W2022972464 hasConceptScore W2022972464C119477230 @default.
• W2022972464 hasConceptScore W2022972464C120806208 @default.
• W2022972464 hasConceptScore W2022972464C127313418 @default.
• W2022972464 hasConceptScore W2022972464C141646446 @default.
• W2022972464 hasConceptScore W2022972464C154200439 @default.
• W2022972464 hasConceptScore W2022972464C165205528 @default.
• W2022972464 hasConceptScore W2022972464C192241223 @default.
• W2022972464 hasConceptScore W2022972464C2524010 @default.
• W2022972464 hasConceptScore W2022972464C2776698055 @default.
• W2022972464 hasConceptScore W2022972464C2777210771 @default.
• W2022972464 hasConceptScore W2022972464C2778261408 @default.
• W2022972464 hasConceptScore W2022972464C33923547 @default.
• W2022972464 hasConceptScore W2022972464C36986328 @default.
• W2022972464 hasConceptScore W2022972464C58097730 @default.
• W2022972464 hasConceptScore W2022972464C64174561 @default.
• W2022972464 hasConceptScore W2022972464C77928131 @default.
• W2022972464 hasConceptScore W2022972464C8058405 @default.
• W2022972464 hasConceptScore W2022972464C83176761 @default.
• W2022972464 hasConceptScore W2022972464C90523207 @default.
• W2022972464 hasIssue "21" @default.
• W2022972464 hasLocation W20229724641 @default.
• W2022972464 hasOpenAccess W2022972464 @default.
• W2022972464 hasPrimaryLocation W20229724641 @default.
• W2022972464 hasRelatedWork W1461768338 @default.
• W2022972464 hasRelatedWork W1967053861 @default.
• W2022972464 hasRelatedWork W1975349032 @default.
• W2022972464 hasRelatedWork W2022784417 @default.
• W2022972464 hasRelatedWork W2052628771 @default.
• W2022972464 hasRelatedWork W2084910823 @default.
• W2022972464 hasRelatedWork W2149307505 @default.
• W2022972464 hasRelatedWork W2607167309 @default.
• W2022972464 hasRelatedWork W3087925122 @default.
• W2022972464 hasRelatedWork W3108038271 @default.
• W2022972464 hasVolume "20" @default.
• W2022972464 isParatext "false" @default.
• W2022972464 isRetracted "false" @default.

• next