FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2062556947> ?p ?o ?g. }

• W2062556947 endingPage "263" @default.
• W2062556947 startingPage "251" @default.
• W2062556947 abstract "The Late Carboniferous (∼ 300 Ma) Hillgrove Plutonic Suite is a deformed, fault-bound suite of S-type granitoids in the southern New England Fold Belt of eastern Australia. Large-scale, W-over-E, high-angle, reverse faulting along major crustal shear zones has exhumed high-grade metamorphic terranes such as the Tia and Wongwibinda migmatite complexes, thereby exposing a tilted section of crust. Exhumed lower amphibolite facies mylonite zones within granitoids have been dated by biotite RbSr using both neocrystallized and relict magmatic biotite. Combined, the analyses define a narrow age range of 266-258 Ma, which indicates that faulting and uplift occurred during the Late Permian. Although the initial temperature conditions during shearing were well above the biotite RbSr closure temperature, these mylonites cooled rapidly, as indicated by identical RbSr ages for relict muscovite and biotite in the adjacent Wongwibinda Complex. RbSr biotite ages for granites not directly affected by ductile shearing range from 296 to 256 Ma, the oldest of which is within error of the ∼ 300 Ma emplacement ages given by UPb zircon dating. RbSr ages obtained from relict biotite in lower-grade, greenschist facies mylonites define a wide range of ages (290-271 Ma), similar to the range acquired for the unsheared granites. The data suggest that shearing in the low-grade mylonites took place at, or just below, the biotite RbSr closure temperature. This range of biotite ages, which varies systematically across the fault blocks, reflects the combined effects of slow cooling from 300 Ma, followed by rapid uplift and tilting of the terrane at ∼ 260 Ma. Biotite RbSr ages of less than 250 Ma are only recorded where samples are affected by local static thermal recrystallization associated with intrusion of Triassic granites. The biotite RbSr data place important chronological constraints on the tectonic evolution of the southern New England Fold Belt. Up to 12 km of Late Permian (268-256 Ma) uplift was the culmination of major E–W compression, which involved large-scale dispersal, oroclinal bending and tilting of crustal blocks." @default.
• W2062556947 created "2016-06-24" @default.
• W2062556947 creator A5011556507 @default.
• W2062556947 date "1995-02-01" @default.
• W2062556947 modified "2023-10-14" @default.
• W2062556947 title "Tectonic implications of Rb_Sr biotite ages for the Hillgrove Plutonic Suite, New England Fold Belt, N.S.W., Australia" @default.
• W2062556947 cites W1983249353 @default.
• W2062556947 cites W1992281628 @default.
• W2062556947 cites W2005069119 @default.
• W2062556947 cites W2017604675 @default.
• W2062556947 cites W2041212518 @default.
• W2062556947 cites W2062947585 @default.
• W2062556947 cites W2072812409 @default.
• W2062556947 cites W2075973823 @default.
• W2062556947 cites W2086711061 @default.
• W2062556947 cites W2087698179 @default.
• W2062556947 cites W2132320235 @default.
• W2062556947 cites W2140416858 @default.
• W2062556947 cites W2167350798 @default.
• W2062556947 cites W598439628 @default.
• W2062556947 cites W98888394 @default.
• W2062556947 doi "https://doi.org/10.1016/0301-9268(94)00064-x" @default.
• W2062556947 hasPublicationYear "1995" @default.
• W2062556947 type Work @default.
• W2062556947 sameAs 2062556947 @default.
• W2062556947 citedByCount "39" @default.
• W2062556947 countsByYear W20625569472012 @default.
• W2062556947 countsByYear W20625569472013 @default.
• W2062556947 countsByYear W20625569472014 @default.
• W2062556947 countsByYear W20625569472015 @default.
• W2062556947 countsByYear W20625569472016 @default.
• W2062556947 countsByYear W20625569472017 @default.
• W2062556947 countsByYear W20625569472018 @default.
• W2062556947 countsByYear W20625569472019 @default.
• W2062556947 countsByYear W20625569472020 @default.
• W2062556947 countsByYear W20625569472021 @default.
• W2062556947 countsByYear W20625569472022 @default.
• W2062556947 countsByYear W20625569472023 @default.
• W2062556947 crossrefType "journal-article" @default.
• W2062556947 hasAuthorship W2062556947A5011556507 @default.
• W2062556947 hasConcept C109007969 @default.
• W2062556947 hasConcept C114793014 @default.
• W2062556947 hasConcept C127313418 @default.
• W2062556947 hasConcept C146588470 @default.
• W2062556947 hasConcept C150999391 @default.
• W2062556947 hasConcept C151730666 @default.
• W2062556947 hasConcept C165205528 @default.
• W2062556947 hasConcept C17409809 @default.
• W2062556947 hasConcept C180785854 @default.
• W2062556947 hasConcept C197737763 @default.
• W2062556947 hasConcept C23295444 @default.
• W2062556947 hasConcept C26687426 @default.
• W2062556947 hasConcept C2776698055 @default.
• W2062556947 hasConcept C2777229588 @default.
• W2062556947 hasConcept C2778849375 @default.
• W2062556947 hasConcept C2779870107 @default.
• W2062556947 hasConcept C34122518 @default.
• W2062556947 hasConcept C37045145 @default.
• W2062556947 hasConcept C5900021 @default.
• W2062556947 hasConcept C77928131 @default.
• W2062556947 hasConcept C79927612 @default.
• W2062556947 hasConceptScore W2062556947C109007969 @default.
• W2062556947 hasConceptScore W2062556947C114793014 @default.
• W2062556947 hasConceptScore W2062556947C127313418 @default.
• W2062556947 hasConceptScore W2062556947C146588470 @default.
• W2062556947 hasConceptScore W2062556947C150999391 @default.
• W2062556947 hasConceptScore W2062556947C151730666 @default.
• W2062556947 hasConceptScore W2062556947C165205528 @default.
• W2062556947 hasConceptScore W2062556947C17409809 @default.
• W2062556947 hasConceptScore W2062556947C180785854 @default.
• W2062556947 hasConceptScore W2062556947C197737763 @default.
• W2062556947 hasConceptScore W2062556947C23295444 @default.
• W2062556947 hasConceptScore W2062556947C26687426 @default.
• W2062556947 hasConceptScore W2062556947C2776698055 @default.
• W2062556947 hasConceptScore W2062556947C2777229588 @default.
• W2062556947 hasConceptScore W2062556947C2778849375 @default.
• W2062556947 hasConceptScore W2062556947C2779870107 @default.
• W2062556947 hasConceptScore W2062556947C34122518 @default.
• W2062556947 hasConceptScore W2062556947C37045145 @default.
• W2062556947 hasConceptScore W2062556947C5900021 @default.
• W2062556947 hasConceptScore W2062556947C77928131 @default.
• W2062556947 hasConceptScore W2062556947C79927612 @default.
• W2062556947 hasIssue "1-4" @default.
• W2062556947 hasLocation W20625569471 @default.
• W2062556947 hasOpenAccess W2062556947 @default.
• W2062556947 hasPrimaryLocation W20625569471 @default.
• W2062556947 hasRelatedWork W161046653 @default.
• W2062556947 hasRelatedWork W1976016997 @default.
• W2062556947 hasRelatedWork W2032420025 @default.
• W2062556947 hasRelatedWork W2047752842 @default.
• W2062556947 hasRelatedWork W2062556947 @default.
• W2062556947 hasRelatedWork W2113147579 @default.
• W2062556947 hasRelatedWork W2262291323 @default.
• W2062556947 hasRelatedWork W2361053869 @default.
• W2062556947 hasRelatedWork W2890140889 @default.
• W2062556947 hasRelatedWork W2902850397 @default.
• W2062556947 hasVolume "71" @default.
• W2062556947 isParatext "false" @default.

• next