FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1594875844> ?p ?o ?g. }

• W1594875844 abstract "The Phanerozoic tectonic evolution of the Circum-North Pacific is recorded mainly in the orogenic collages of the Circum-North Pacific mountain belts that separate the North Pacific from the eastern part of the North Asian Craton and the western part of the North American Craton. These collages consist of tectonostratigraphic terranes that are composed of fragments of igneous arcs, accretionary-wedge and subduction-zone complexes, passive continental margins, and cratons; they are overlapped by continental-margin-arc and sedimentary-basin assemblages. The geologic history of the terranes and overlap assemblages is highly complex because of postaccretionary dismemberment and translation during strike-slip faulting that occurred subparallel to continental margins.We analyze the complex tectonics of this region by the following steps. (1) We assign tectonic environments for the orogenic collages from regional compilation and synthesis of stratigraphic and faunal data. The types of tectonic environments include cratonal, passive continental margin, metamorphosed continental margin, continental-margin arc, island arc, oceanic crust, seamount, ophiolite, accretionary wedge, subduction zone, turbidite basin, and metamorphic. (2) We make correlations between terranes. (3) We group coeval terranes into a single tectonic origin, for example, a single island arc or subduction zone. (4) We group igneous-arc and subduction- zone terranes, which are interpreted as being tectonically linked, into coeval, curvilinear arc/subduction-zone complexes. (5) We interpret the original positions of terranes, using geologic, faunal, and paleomagnetic data. (6) We construct the paths of tectonic migration. Six processes overlapping in time were responsible for most of the complexities of the collage of terranes and overlap assemblages around the Circum-North Pacific, as follows. (1) During the Late Proterozoic, Late Devonian, and Early Carboniferous, major periods of rifting occurred along the ancestral margins of present-day Northeast Asia and northwestern North America. The rifting resulted in the fragmentation of each continent and the formation of cratonal and passive continental-margin terranes that eventually migrated and accreted to other sites along the evolving margins of the original or adjacent continents. (2) From about the Late Triassic through the mid-Cretaceous, a succession of island arcs and tectonically paired subduction zones formed near the continental margins. (3) From about mainly the mid-Cretaceous through the present, a succession of igneous arcs and tectonically paired subduction zones formed along the continental margins. (4) From about the Jurassic to the present, oblique convergence and rotations caused orogenparallel sinistral and then dextral displacements within the upper-plate margins of cratons that have become Northeast Asia and North America. The oblique convergences and rotations resulted in the fragmentation, displacement, and duplication of formerly more nearly continuous arcs, subduction zones, and passive continental margins. These fragments were subsequently accreted along the expanding continental margins. (5) From the Early Jurassic through Tertiary, movement of the upper continental plates toward subduction zones resulted in strong plate coupling and accretion of the former island arcs and subduction zones to the continental margins. Accretions were accompanied and followed by crustal thickening, anatexis, metamorphism, and uplift. The accretions resulted in substantial growth of the North Asian and North American Continents. (6) During the middle and late Cenozoic, oblique to orthogonal convergence of the Pacifi c plate with present-day Alaska and Northeast Asia resulted in formation of the modern-day ring of volcanoes around the Circum-North Pacific. Oblique convergence between the Pacific plate and Alaska also resulted in major dextral-slip faulting in interior and southern Alaska and along the western p" @default.
• W1594875844 created "2016-06-24" @default.
• W1594875844 creator A5001627034 @default.
• W1594875844 creator A5006887556 @default.
• W1594875844 creator A5018177372 @default.
• W1594875844 creator A5021153908 @default.
• W1594875844 creator A5023355381 @default.
• W1594875844 creator A5029613970 @default.
• W1594875844 creator A5033875284 @default.
• W1594875844 creator A5052526066 @default.
• W1594875844 creator A5074865450 @default.
• W1594875844 date "2000-01-01" @default.
• W1594875844 modified "2023-10-11" @default.
• W1594875844 title "Phanerozoic tectonic evolution of the Circum-North Pacific" @default.
• W1594875844 doi "https://doi.org/10.3133/pp1626" @default.
• W1594875844 hasPublicationYear "2000" @default.
• W1594875844 type Work @default.
• W1594875844 sameAs 1594875844 @default.
• W1594875844 citedByCount "109" @default.
• W1594875844 countsByYear W15948758442012 @default.
• W1594875844 countsByYear W15948758442013 @default.
• W1594875844 countsByYear W15948758442014 @default.
• W1594875844 countsByYear W15948758442015 @default.
• W1594875844 countsByYear W15948758442016 @default.
• W1594875844 countsByYear W15948758442017 @default.
• W1594875844 countsByYear W15948758442018 @default.
• W1594875844 countsByYear W15948758442019 @default.
• W1594875844 countsByYear W15948758442020 @default.
• W1594875844 countsByYear W15948758442021 @default.
• W1594875844 countsByYear W15948758442022 @default.
• W1594875844 countsByYear W15948758442023 @default.
• W1594875844 crossrefType "journal-article" @default.
• W1594875844 hasAuthorship W1594875844A5001627034 @default.
• W1594875844 hasAuthorship W1594875844A5006887556 @default.
• W1594875844 hasAuthorship W1594875844A5018177372 @default.
• W1594875844 hasAuthorship W1594875844A5021153908 @default.
• W1594875844 hasAuthorship W1594875844A5023355381 @default.
• W1594875844 hasAuthorship W1594875844A5029613970 @default.
• W1594875844 hasAuthorship W1594875844A5033875284 @default.
• W1594875844 hasAuthorship W1594875844A5052526066 @default.
• W1594875844 hasAuthorship W1594875844A5074865450 @default.
• W1594875844 hasBestOaLocation W15948758442 @default.
• W1594875844 hasConcept C119477230 @default.
• W1594875844 hasConcept C127313418 @default.
• W1594875844 hasConcept C141646446 @default.
• W1594875844 hasConcept C147717901 @default.
• W1594875844 hasConcept C150999391 @default.
• W1594875844 hasConcept C151730666 @default.
• W1594875844 hasConcept C154200439 @default.
• W1594875844 hasConcept C165205528 @default.
• W1594875844 hasConcept C192717286 @default.
• W1594875844 hasConcept C1965285 @default.
• W1594875844 hasConcept C201867031 @default.
• W1594875844 hasConcept C23923706 @default.
• W1594875844 hasConcept C44140439 @default.
• W1594875844 hasConcept C58097730 @default.
• W1594875844 hasConcept C63379926 @default.
• W1594875844 hasConcept C77928131 @default.
• W1594875844 hasConceptScore W1594875844C119477230 @default.
• W1594875844 hasConceptScore W1594875844C127313418 @default.
• W1594875844 hasConceptScore W1594875844C141646446 @default.
• W1594875844 hasConceptScore W1594875844C147717901 @default.
• W1594875844 hasConceptScore W1594875844C150999391 @default.
• W1594875844 hasConceptScore W1594875844C151730666 @default.
• W1594875844 hasConceptScore W1594875844C154200439 @default.
• W1594875844 hasConceptScore W1594875844C165205528 @default.
• W1594875844 hasConceptScore W1594875844C192717286 @default.
• W1594875844 hasConceptScore W1594875844C1965285 @default.
• W1594875844 hasConceptScore W1594875844C201867031 @default.
• W1594875844 hasConceptScore W1594875844C23923706 @default.
• W1594875844 hasConceptScore W1594875844C44140439 @default.
• W1594875844 hasConceptScore W1594875844C58097730 @default.
• W1594875844 hasConceptScore W1594875844C63379926 @default.
• W1594875844 hasConceptScore W1594875844C77928131 @default.
• W1594875844 hasLocation W15948758441 @default.
• W1594875844 hasLocation W15948758442 @default.
• W1594875844 hasOpenAccess W1594875844 @default.
• W1594875844 hasPrimaryLocation W15948758441 @default.
• W1594875844 hasRelatedWork W1594875844 @default.
• W1594875844 hasRelatedWork W1979820932 @default.
• W1594875844 hasRelatedWork W3119338171 @default.
• W1594875844 hasRelatedWork W3162523750 @default.
• W1594875844 hasRelatedWork W3168976727 @default.
• W1594875844 hasRelatedWork W4200566686 @default.
• W1594875844 hasRelatedWork W4205114424 @default.
• W1594875844 hasRelatedWork W4246287523 @default.
• W1594875844 hasRelatedWork W4324358762 @default.
• W1594875844 hasRelatedWork W3016024417 @default.
• W1594875844 isParatext "false" @default.
• W1594875844 isRetracted "false" @default.
• W1594875844 magId "1594875844" @default.
• W1594875844 workType "article" @default.