Matches in SemOpenAlex for { <https://semopenalex.org/work/W1983338920> ?p ?o ?g. }
- W1983338920 endingPage "492" @default.
- W1983338920 startingPage "483" @default.
- W1983338920 abstract "The traditional view of ‘paired’ metamorphic belts forming adjacent to each other in a common arc–trench subduction system is challenged, and it is suggested that an alternative view based on terrane tectonics is more consistent with the geological evidence. For the low-P/T ratio Ryoke metamorphic belt of southwest Japan, an origin by ridge subduction is consistent with the geological evidence and results of numerical modeling by Iwamori. However, the parallel high-P/T ratio Sanbagawa metamorphic belt most likely was translated northeast after the Ryoke ridge subduction event and was juxtaposed against the low-P/T ratio metamorphic belt during the Late Cretaceous, causing progressive southwest to northeast exhumation and diachronous cooling of the low-P/T ratio metamorphic rocks. Similarly, accretion by underplating in the Shimanto belt likely caused exhumation and cooling of the high-P/T ratio metamorphic rocks of the Sanbagawa and Northern Chichibu belts concurrently with exhumation and cooling of the Ryoke belt. As a result, the prograde metamorphic evolution of the Ryoke and Sanbagawa belts cannot be modeled as a ‘pair’ that formed in situ; the application of results of numerical models to the origin of plate margin metamorphic belts must be based on an understanding of the geology. In the model presented by Iwamori, the low-P/T ratio metamorphism and high-P/T ratio metamorphism are ascribed to the same ridge subduction event in a common trench system. Although such a scenario may produce lower-P to higher-P metamorphism in the inboard direction, it cannot generate a high-P/T ratio belt outboard of a low-P/T ratio belt." @default.
- W1983338920 created "2016-06-24" @default.
- W1983338920 creator A5015954930 @default.
- W1983338920 date "2002-06-01" @default.
- W1983338920 modified "2023-09-26" @default.
- W1983338920 title "Plate margin processes and ‘paired’ metamorphic belts in Japan: Comment on ‘Thermal effects of ridge subduction and its implications for the origin of granitic batholith and paired metamorphic belts’ by H. Iwamori" @default.
- W1983338920 cites W1562392071 @default.
- W1983338920 cites W1567015154 @default.
- W1983338920 cites W1582958040 @default.
- W1983338920 cites W1963800524 @default.
- W1983338920 cites W1977662287 @default.
- W1983338920 cites W1980662722 @default.
- W1983338920 cites W1981230204 @default.
- W1983338920 cites W1981790870 @default.
- W1983338920 cites W1983616064 @default.
- W1983338920 cites W1985026732 @default.
- W1983338920 cites W1996771811 @default.
- W1983338920 cites W1998596829 @default.
- W1983338920 cites W2002988964 @default.
- W1983338920 cites W2005712453 @default.
- W1983338920 cites W2009766250 @default.
- W1983338920 cites W2023430719 @default.
- W1983338920 cites W2028144742 @default.
- W1983338920 cites W2028203656 @default.
- W1983338920 cites W2030866738 @default.
- W1983338920 cites W2036727400 @default.
- W1983338920 cites W2037938663 @default.
- W1983338920 cites W2044793733 @default.
- W1983338920 cites W2045475865 @default.
- W1983338920 cites W2053504990 @default.
- W1983338920 cites W2057026910 @default.
- W1983338920 cites W2057864838 @default.
- W1983338920 cites W2064197334 @default.
- W1983338920 cites W2069462222 @default.
- W1983338920 cites W2071172609 @default.
- W1983338920 cites W2072114070 @default.
- W1983338920 cites W2076001655 @default.
- W1983338920 cites W2076682814 @default.
- W1983338920 cites W2077192281 @default.
- W1983338920 cites W2078218892 @default.
- W1983338920 cites W2081029245 @default.
- W1983338920 cites W2081681324 @default.
- W1983338920 cites W2090450139 @default.
- W1983338920 cites W2093317589 @default.
- W1983338920 cites W2094182452 @default.
- W1983338920 cites W2095080287 @default.
- W1983338920 cites W2107076162 @default.
- W1983338920 cites W2128883863 @default.
- W1983338920 cites W2130439244 @default.
- W1983338920 cites W2136288089 @default.
- W1983338920 cites W2164495831 @default.
- W1983338920 cites W2179853145 @default.
- W1983338920 cites W2314778238 @default.
- W1983338920 cites W2332383354 @default.
- W1983338920 cites W2333754923 @default.
- W1983338920 cites W4245388509 @default.
- W1983338920 cites W4293860446 @default.
- W1983338920 doi "https://doi.org/10.1016/s0012-821x(02)00582-4" @default.
- W1983338920 hasPublicationYear "2002" @default.
- W1983338920 type Work @default.
- W1983338920 sameAs 1983338920 @default.
- W1983338920 citedByCount "20" @default.
- W1983338920 countsByYear W19833389202012 @default.
- W1983338920 countsByYear W19833389202014 @default.
- W1983338920 countsByYear W19833389202016 @default.
- W1983338920 countsByYear W19833389202018 @default.
- W1983338920 countsByYear W19833389202019 @default.
- W1983338920 countsByYear W19833389202021 @default.
- W1983338920 countsByYear W19833389202023 @default.
- W1983338920 crossrefType "journal-article" @default.
- W1983338920 hasAuthorship W1983338920A5015954930 @default.
- W1983338920 hasConcept C109007969 @default.
- W1983338920 hasConcept C112764850 @default.
- W1983338920 hasConcept C127313418 @default.
- W1983338920 hasConcept C136137745 @default.
- W1983338920 hasConcept C146588470 @default.
- W1983338920 hasConcept C150999391 @default.
- W1983338920 hasConcept C151730666 @default.
- W1983338920 hasConcept C165205528 @default.
- W1983338920 hasConcept C166591241 @default.
- W1983338920 hasConcept C17409809 @default.
- W1983338920 hasConcept C26687426 @default.
- W1983338920 hasConcept C2776340010 @default.
- W1983338920 hasConcept C32277403 @default.
- W1983338920 hasConcept C58097730 @default.
- W1983338920 hasConcept C5900021 @default.
- W1983338920 hasConcept C63014310 @default.
- W1983338920 hasConcept C77928131 @default.
- W1983338920 hasConcept C79927612 @default.
- W1983338920 hasConcept C95628711 @default.
- W1983338920 hasConceptScore W1983338920C109007969 @default.
- W1983338920 hasConceptScore W1983338920C112764850 @default.
- W1983338920 hasConceptScore W1983338920C127313418 @default.
- W1983338920 hasConceptScore W1983338920C136137745 @default.
- W1983338920 hasConceptScore W1983338920C146588470 @default.
- W1983338920 hasConceptScore W1983338920C150999391 @default.
- W1983338920 hasConceptScore W1983338920C151730666 @default.
- W1983338920 hasConceptScore W1983338920C165205528 @default.