FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2003484054> ?p ?o ?g. }

• W2003484054 endingPage "87" @default.
• W2003484054 startingPage "57" @default.
• W2003484054 abstract "Abstract Subduction zones with deep seismicity are believed to be associated with the descending branches of convective flows in the mantle and are subordinated to them. Therefore, the position of subduction zones can be considered as relatively fixed with respect to the steady-state system of convective flows. The lithospheric plate overhanging a subduction zone (as a rule of continental type) may: 1. (1) either move away from the subduction zone; or 2. (2) move onto it. In the first case extensional conditions originate behind the subduction zone and the new oceanic crust of back-arc basins forms. In the second case active Andean-type continental margins with thickening of the crust and lithosphere are observed. Behind the majority of volcanic island-arcs, along the boundary with marginal-sea basins, independent shallow seismicity belts can be traced. They are parallel to the main seismicity belts coinciding with the Benioff zones. The seismicity belts frame island-arc microplates. Island-arc microplates are assumed to be a frame of reference to calculate relative movements of the consuming and overhanging plates. Using slip vector azimuths for shallow seismicity belts in the frontal parts of the Kurile, Japan, Izu-Bonin, Mariana and Tonga—Kermadec arcs, the position of the pole of rotation of the Pacific plate with respect to the western Pacific island-arc microplates was computed. Its coordinates are 66.1°N, 119.2°W. From the global closure of plate movements it has been determined that for the past 10 m.y. the Eurasian and Indian plates have been moving away from the Western Pacific island-arc system, both rotating clockwise, around poles at 31.1°N, 164.2°W and 1.3°S, 157.5°W, respectively. This provides for the opening of the back-arc basins. At the same time South America is moving onto the subduction zone at the rate of 4 cm/yr. Some “hot spots”, such as Hawaiian, Tibesti, and those of the South Atlantic, are moving relative to the island-arc system at a very low rate, viz. 0.5–0.7 cm/yr. Presumably, the western Pacific subduction zone and “hot spots” form a single frame of reference which can generally be used for the analysis of absolute motions." @default.
• W2003484054 created "2016-06-24" @default.
• W2003484054 creator A5032771192 @default.
• W2003484054 creator A5036845115 @default.
• W2003484054 date "1981-04-01" @default.
• W2003484054 modified "2023-09-27" @default.
• W2003484054 title "Movement of lithospheric plates relative to subduction zones: Formation of marginal seas and active continental margins" @default.
• W2003484054 cites W1964243252 @default.
• W2003484054 cites W1969397327 @default.
• W2003484054 cites W1978866236 @default.
• W2003484054 cites W1983508465 @default.
• W2003484054 cites W1992559108 @default.
• W2003484054 cites W1993082095 @default.
• W2003484054 cites W2002674588 @default.
• W2003484054 cites W2003164357 @default.
• W2003484054 cites W2004501456 @default.
• W2003484054 cites W2005419403 @default.
• W2003484054 cites W2009930154 @default.
• W2003484054 cites W2018881505 @default.
• W2003484054 cites W2021926110 @default.
• W2003484054 cites W2030712516 @default.
• W2003484054 cites W2034322653 @default.
• W2003484054 cites W2039055754 @default.
• W2003484054 cites W2042559327 @default.
• W2003484054 cites W2048280755 @default.
• W2003484054 cites W2049007541 @default.
• W2003484054 cites W2050456239 @default.
• W2003484054 cites W2052176865 @default.
• W2003484054 cites W2053658624 @default.
• W2003484054 cites W2055364427 @default.
• W2003484054 cites W2061211721 @default.
• W2003484054 cites W2066711037 @default.
• W2003484054 cites W2072829874 @default.
• W2003484054 cites W2074105632 @default.
• W2003484054 cites W2077238091 @default.
• W2003484054 cites W2078435365 @default.
• W2003484054 cites W2087385680 @default.
• W2003484054 cites W2097800673 @default.
• W2003484054 cites W2098866791 @default.
• W2003484054 cites W2099719806 @default.
• W2003484054 cites W2108073717 @default.
• W2003484054 cites W2110164257 @default.
• W2003484054 cites W2116894649 @default.
• W2003484054 cites W2127454332 @default.
• W2003484054 cites W2131279760 @default.
• W2003484054 cites W2135691959 @default.
• W2003484054 cites W2144388466 @default.
• W2003484054 cites W2146282982 @default.
• W2003484054 cites W2147468306 @default.
• W2003484054 cites W2149587025 @default.
• W2003484054 cites W2160361224 @default.
• W2003484054 cites W2166167505 @default.
• W2003484054 cites W2169730990 @default.
• W2003484054 cites W2170969682 @default.
• W2003484054 cites W2338336510 @default.
• W2003484054 doi "https://doi.org/10.1016/0040-1951(81)90128-1" @default.
• W2003484054 hasPublicationYear "1981" @default.
• W2003484054 type Work @default.
• W2003484054 sameAs 2003484054 @default.
• W2003484054 citedByCount "15" @default.
• W2003484054 crossrefType "journal-article" @default.
• W2003484054 hasAuthorship W2003484054A5032771192 @default.
• W2003484054 hasAuthorship W2003484054A5036845115 @default.
• W2003484054 hasConcept C107038049 @default.
• W2003484054 hasConcept C111368507 @default.
• W2003484054 hasConcept C127313418 @default.
• W2003484054 hasConcept C138885662 @default.
• W2003484054 hasConcept C165205528 @default.
• W2003484054 hasConcept C16942324 @default.
• W2003484054 hasConcept C184751465 @default.
• W2003484054 hasConcept C201633675 @default.
• W2003484054 hasConcept C201867031 @default.
• W2003484054 hasConcept C2780226923 @default.
• W2003484054 hasConcept C50682988 @default.
• W2003484054 hasConcept C58097730 @default.
• W2003484054 hasConcept C77928131 @default.
• W2003484054 hasConceptScore W2003484054C107038049 @default.
• W2003484054 hasConceptScore W2003484054C111368507 @default.
• W2003484054 hasConceptScore W2003484054C127313418 @default.
• W2003484054 hasConceptScore W2003484054C138885662 @default.
• W2003484054 hasConceptScore W2003484054C165205528 @default.
• W2003484054 hasConceptScore W2003484054C16942324 @default.
• W2003484054 hasConceptScore W2003484054C184751465 @default.
• W2003484054 hasConceptScore W2003484054C201633675 @default.
• W2003484054 hasConceptScore W2003484054C201867031 @default.
• W2003484054 hasConceptScore W2003484054C2780226923 @default.
• W2003484054 hasConceptScore W2003484054C50682988 @default.
• W2003484054 hasConceptScore W2003484054C58097730 @default.
• W2003484054 hasConceptScore W2003484054C77928131 @default.
• W2003484054 hasIssue "1-2" @default.
• W2003484054 hasLocation W20034840541 @default.
• W2003484054 hasOpenAccess W2003484054 @default.
• W2003484054 hasPrimaryLocation W20034840541 @default.
• W2003484054 hasRelatedWork W2007304281 @default.
• W2003484054 hasRelatedWork W2043856024 @default.
• W2003484054 hasRelatedWork W2156916342 @default.
• W2003484054 hasRelatedWork W2188936146 @default.
• W2003484054 hasRelatedWork W2265213580 @default.

• next