Matches in SemOpenAlex for { <https://semopenalex.org/work/W2046609097> ?p ?o ?g. }
- W2046609097 endingPage "426" @default.
- W2046609097 startingPage "403" @default.
- W2046609097 abstract "Five generations of structure (D1‐D5) have been recognized in the Early Archaean supracrustal gneisses in the Fyfe Hills‐Khmara Bay region in Enderby Land, East Antarctica. The D1, D2 and D3 events comprise the Napier structural episode. They resulted in pervasive deformation during Archaean granulite facies metamorphism, and predated the intrusion of the Middle Proterozoic Amundsen dykes. The Napier metamorphic culmination was broadly coeval with, but outlasted both, D1 and D2. D3 occurred during waning granulite facies metamorphism. The D4 and D5 events comprise the Rayner structural episode, the effects of which are largely restricted to amphibolite facies retrograde shear zones in which the Amundsen dykes are deformed. The Napier Structural Episode is characterized by: (i) mesoscopic, isoclinal, recumbent, F1 folds which formed during intense deformation accompanying the prograde burial of the gneissic sequence; (ii) large scale, tieht to isoclinal, reclined F2 folds formed at deep crustal levels; and (iii) large scale, non‐cylindrical, asymmetric, upright F3 folds formed in response to differential vertical movements during the final stages of stabilization of the gneissic sequence. The development of a pervasive mesoscopic gneissic layering associated with the Napier structures is attributed to a variety of processes, only some of which are related to deformation mechanisms. The Rayner structures are restricted to amphibolite grade high strain zones which formed in response to displacements between essentially rigid blocks of granulite. Progressive localization of D4 and D5 structures within the retrograde zones, ultimately resulting in the development of pseudotachylite, reflects deformation at successively higher crustal levels during the excavation of the gneissic sequence." @default.
- W2046609097 created "2016-06-24" @default.
- W2046609097 creator A5026326429 @default.
- W2046609097 creator A5048584901 @default.
- W2046609097 date "1984-12-01" @default.
- W2046609097 modified "2023-09-29" @default.
- W2046609097 title "The structural evolution of the Fyfe Hills‐Khmara Bay region, Enderby Land, East Antarctica" @default.
- W2046609097 cites W1974880152 @default.
- W2046609097 cites W1986367860 @default.
- W2046609097 cites W1993510565 @default.
- W2046609097 cites W1999680324 @default.
- W2046609097 cites W2003546631 @default.
- W2046609097 cites W2021277960 @default.
- W2046609097 cites W2022373295 @default.
- W2046609097 cites W2024549725 @default.
- W2046609097 cites W2026207505 @default.
- W2046609097 cites W2029370166 @default.
- W2046609097 cites W2040138445 @default.
- W2046609097 cites W2041716321 @default.
- W2046609097 cites W2043998613 @default.
- W2046609097 cites W2047136573 @default.
- W2046609097 cites W2052820815 @default.
- W2046609097 cites W2067019494 @default.
- W2046609097 cites W2071904071 @default.
- W2046609097 cites W2080506700 @default.
- W2046609097 cites W2090936331 @default.
- W2046609097 cites W2110605607 @default.
- W2046609097 cites W2122773833 @default.
- W2046609097 cites W2138860509 @default.
- W2046609097 cites W2160527958 @default.
- W2046609097 cites W2164683099 @default.
- W2046609097 cites W4250749882 @default.
- W2046609097 doi "https://doi.org/10.1080/08120098408729301" @default.
- W2046609097 hasPublicationYear "1984" @default.
- W2046609097 type Work @default.
- W2046609097 sameAs 2046609097 @default.
- W2046609097 citedByCount "57" @default.
- W2046609097 countsByYear W20466090972012 @default.
- W2046609097 countsByYear W20466090972013 @default.
- W2046609097 countsByYear W20466090972015 @default.
- W2046609097 countsByYear W20466090972016 @default.
- W2046609097 countsByYear W20466090972017 @default.
- W2046609097 countsByYear W20466090972020 @default.
- W2046609097 countsByYear W20466090972021 @default.
- W2046609097 crossrefType "journal-article" @default.
- W2046609097 hasAuthorship W2046609097A5026326429 @default.
- W2046609097 hasAuthorship W2046609097A5048584901 @default.
- W2046609097 hasConcept C109007969 @default.
- W2046609097 hasConcept C112764850 @default.
- W2046609097 hasConcept C114793014 @default.
- W2046609097 hasConcept C127313418 @default.
- W2046609097 hasConcept C127413603 @default.
- W2046609097 hasConcept C146588470 @default.
- W2046609097 hasConcept C149347711 @default.
- W2046609097 hasConcept C151730666 @default.
- W2046609097 hasConcept C171701179 @default.
- W2046609097 hasConcept C17409809 @default.
- W2046609097 hasConcept C18142444 @default.
- W2046609097 hasConcept C23295444 @default.
- W2046609097 hasConcept C26687426 @default.
- W2046609097 hasConcept C2780733770 @default.
- W2046609097 hasConcept C2781150389 @default.
- W2046609097 hasConcept C53942344 @default.
- W2046609097 hasConcept C5900021 @default.
- W2046609097 hasConcept C77928131 @default.
- W2046609097 hasConcept C78519656 @default.
- W2046609097 hasConcept C79927612 @default.
- W2046609097 hasConcept C98742433 @default.
- W2046609097 hasConceptScore W2046609097C109007969 @default.
- W2046609097 hasConceptScore W2046609097C112764850 @default.
- W2046609097 hasConceptScore W2046609097C114793014 @default.
- W2046609097 hasConceptScore W2046609097C127313418 @default.
- W2046609097 hasConceptScore W2046609097C127413603 @default.
- W2046609097 hasConceptScore W2046609097C146588470 @default.
- W2046609097 hasConceptScore W2046609097C149347711 @default.
- W2046609097 hasConceptScore W2046609097C151730666 @default.
- W2046609097 hasConceptScore W2046609097C171701179 @default.
- W2046609097 hasConceptScore W2046609097C17409809 @default.
- W2046609097 hasConceptScore W2046609097C18142444 @default.
- W2046609097 hasConceptScore W2046609097C23295444 @default.
- W2046609097 hasConceptScore W2046609097C26687426 @default.
- W2046609097 hasConceptScore W2046609097C2780733770 @default.
- W2046609097 hasConceptScore W2046609097C2781150389 @default.
- W2046609097 hasConceptScore W2046609097C53942344 @default.
- W2046609097 hasConceptScore W2046609097C5900021 @default.
- W2046609097 hasConceptScore W2046609097C77928131 @default.
- W2046609097 hasConceptScore W2046609097C78519656 @default.
- W2046609097 hasConceptScore W2046609097C79927612 @default.
- W2046609097 hasConceptScore W2046609097C98742433 @default.
- W2046609097 hasIssue "4" @default.
- W2046609097 hasLocation W20466090971 @default.
- W2046609097 hasOpenAccess W2046609097 @default.
- W2046609097 hasPrimaryLocation W20466090971 @default.
- W2046609097 hasRelatedWork W1973766493 @default.
- W2046609097 hasRelatedWork W1974274983 @default.
- W2046609097 hasRelatedWork W2009612684 @default.
- W2046609097 hasRelatedWork W2012258136 @default.
- W2046609097 hasRelatedWork W204150766 @default.