FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2007355072> ?p ?o ?g. }

• W2007355072 endingPage "536" @default.
• W2007355072 startingPage "523" @default.
• W2007355072 abstract "The Sanbagawa high-pressure schists from central Shikoku in Southwest Japan have experienced high-strain ductile deformation during exhumation and cooling. This study examines the effects of high-strain ductile deformation on K–Ar ages of phengites on the basis of fabric, chemistry and K–Ar ages of phengites from the pelitic, psammitic and quartzose (or albitic) schists collected from the same outcrop in the albite–biotite zone. Phengites in the pelitic and psammitic schists generally occur forming aggregates consisting of fine-grained phengite crystals and are extremely fine-grained in domains close to relatively rigid garnet and albite porphyroblasts, indicating that deformation-induced grain-size reduction had taken place in phengite during the ductile deformation accompanying the exhumation of host schists. We suggest that the grain-size reduction of phengite is due to strain-induced recrystallization or dynamic recrystallization. The matrix phengites in schists are chemically heterogeneous on the thin-section scale but the phengites from pelitic and psammitic schists from the same outcrop have similar chemical range. Phengite included in garnet has a high Si value and its Na/(Na + K) and Mg/(Mg + Fe) ratios are significantly low in comparison with those in matrix. The phengite included in garnet records the chemistry in equilibrium with other major silicate phases during the higher pressure stage of the P–T–t history of the schists. In contrast, the matrix phengites having low Si values are likely to have been formed during retrograde metamorphism in extremely restricted equilibrium domains. The two or three different types of schists from the same outcrop, which have a similar grain size of phengite, have similar K–Ar ages, suggesting that the closure temperature does not depend on chemistry. However, the hematite-rich quartzose schist with strong grain-size reduction of both phengite and quartz has a significantly younger K–Ar phengite age than the pelitic and quartzose schists in the same outcrop that do not show grain-size reduction. We suggest that the exhumation tectonics of the schists, which have experienced strong ductile deformation at temperatures less than ~350°C, played an important role resulting in the observed variation in age." @default.
• W2007355072 created "2016-06-24" @default.
• W2007355072 creator A5050106388 @default.
• W2007355072 creator A5070709438 @default.
• W2007355072 date "1999-12-01" @default.
• W2007355072 modified "2023-10-18" @default.
• W2007355072 title "K-Ar age-chemistry-fabric relations of phengite from the Sanbagawa high-pressure schists, Japan" @default.
• W2007355072 cites W1495508698 @default.
• W2007355072 cites W1963800524 @default.
• W2007355072 cites W1974571097 @default.
• W2007355072 cites W1975063615 @default.
• W2007355072 cites W1981480622 @default.
• W2007355072 cites W1997283245 @default.
• W2007355072 cites W1998596829 @default.
• W2007355072 cites W2008937734 @default.
• W2007355072 cites W2012576895 @default.
• W2007355072 cites W2016619260 @default.
• W2007355072 cites W2018827751 @default.
• W2007355072 cites W2028203656 @default.
• W2007355072 cites W2033178018 @default.
• W2007355072 cites W2057026910 @default.
• W2007355072 cites W2069462222 @default.
• W2007355072 cites W2078459725 @default.
• W2007355072 cites W2084138021 @default.
• W2007355072 cites W2124254763 @default.
• W2007355072 cites W2145604970 @default.
• W2007355072 cites W2315525270 @default.
• W2007355072 cites W2328326581 @default.
• W2007355072 cites W2331111374 @default.
• W2007355072 cites W2332383354 @default.
• W2007355072 cites W56570304 @default.
• W2007355072 doi "https://doi.org/10.1046/j.1440-1738.1999.00253.x" @default.
• W2007355072 hasPublicationYear "1999" @default.
• W2007355072 type Work @default.
• W2007355072 sameAs 2007355072 @default.
• W2007355072 citedByCount "23" @default.
• W2007355072 countsByYear W20073550722012 @default.
• W2007355072 countsByYear W20073550722013 @default.
• W2007355072 countsByYear W20073550722014 @default.
• W2007355072 countsByYear W20073550722015 @default.
• W2007355072 countsByYear W20073550722016 @default.
• W2007355072 countsByYear W20073550722017 @default.
• W2007355072 countsByYear W20073550722020 @default.
• W2007355072 countsByYear W20073550722021 @default.
• W2007355072 crossrefType "journal-article" @default.
• W2007355072 hasAuthorship W2007355072A5050106388 @default.
• W2007355072 hasAuthorship W2007355072A5070709438 @default.
• W2007355072 hasConcept C101139013 @default.
• W2007355072 hasConcept C112764850 @default.
• W2007355072 hasConcept C127313418 @default.
• W2007355072 hasConcept C151730666 @default.
• W2007355072 hasConcept C165205528 @default.
• W2007355072 hasConcept C171710264 @default.
• W2007355072 hasConcept C173347748 @default.
• W2007355072 hasConcept C17409809 @default.
• W2007355072 hasConcept C195702682 @default.
• W2007355072 hasConcept C26687426 @default.
• W2007355072 hasConcept C2775859737 @default.
• W2007355072 hasConcept C2777054243 @default.
• W2007355072 hasConcept C2777229588 @default.
• W2007355072 hasConcept C2779870107 @default.
• W2007355072 hasConcept C58097730 @default.
• W2007355072 hasConcept C5900021 @default.
• W2007355072 hasConcept C77928131 @default.
• W2007355072 hasConceptScore W2007355072C101139013 @default.
• W2007355072 hasConceptScore W2007355072C112764850 @default.
• W2007355072 hasConceptScore W2007355072C127313418 @default.
• W2007355072 hasConceptScore W2007355072C151730666 @default.
• W2007355072 hasConceptScore W2007355072C165205528 @default.
• W2007355072 hasConceptScore W2007355072C171710264 @default.
• W2007355072 hasConceptScore W2007355072C173347748 @default.
• W2007355072 hasConceptScore W2007355072C17409809 @default.
• W2007355072 hasConceptScore W2007355072C195702682 @default.
• W2007355072 hasConceptScore W2007355072C26687426 @default.
• W2007355072 hasConceptScore W2007355072C2775859737 @default.
• W2007355072 hasConceptScore W2007355072C2777054243 @default.
• W2007355072 hasConceptScore W2007355072C2777229588 @default.
• W2007355072 hasConceptScore W2007355072C2779870107 @default.
• W2007355072 hasConceptScore W2007355072C58097730 @default.
• W2007355072 hasConceptScore W2007355072C5900021 @default.
• W2007355072 hasConceptScore W2007355072C77928131 @default.
• W2007355072 hasIssue "4" @default.
• W2007355072 hasLocation W20073550721 @default.
• W2007355072 hasOpenAccess W2007355072 @default.
• W2007355072 hasPrimaryLocation W20073550721 @default.
• W2007355072 hasRelatedWork W2049386485 @default.
• W2007355072 hasRelatedWork W2069437485 @default.
• W2007355072 hasRelatedWork W2078565135 @default.
• W2007355072 hasRelatedWork W2088804581 @default.
• W2007355072 hasRelatedWork W2124820105 @default.
• W2007355072 hasRelatedWork W2155961274 @default.
• W2007355072 hasRelatedWork W2314213274 @default.
• W2007355072 hasRelatedWork W2318595290 @default.
• W2007355072 hasRelatedWork W2375249931 @default.
• W2007355072 hasRelatedWork W3150824885 @default.
• W2007355072 hasVolume "8" @default.
• W2007355072 isParatext "false" @default.
• W2007355072 isRetracted "false" @default.

• next