FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2015496622> ?p ?o ?g. }

• W2015496622 endingPage "153" @default.
• W2015496622 startingPage "133" @default.
• W2015496622 abstract "The Pelagonian Zone of the Hellenides, which occurs in the northwestern Aegean region of the Eastern Mediterranean, contains remnants of a high-pressure metamorphic belt which subsequently underwent localized reworking during low-temperature deformational events. Formation of Alpine deformational structures in the Ossa Massif (northern Pelagonian Zone) occurred at metamorphic temperatures which failed to reset most pre-Alpine 40Ar/39Ar cooling ages in muscovite porphyroclasts. The low metamorphic temperatures at Alpine times have preserved the argon isotopic signature in white mica bearing deformational structures, which allows direct dating of these structures and refinement of the Alpine tectonic history in the region. After separation of carefully selected and characterized mica generations, application of sensitive 40Ar/39Ar laserprobe dating has resulted in a continuous record of the early Alpine tectonic history of the Ossa Massif from the Early Cretaceous well into the Eocene. The early Alpine history of the Ossa Massif records cooling of basement thrust slices, which are mostly Hercynian granites and metamorphics, below ca. 350°C by 100 Ma, while lower tectonostratigraphic levels of the basement had already cooled below these temperatures at around ca. 285 Ma. Blueschist facies mylonite fabrics, related to a top-to-ENE direction of tectonic transport, yield ages as old as 84.5±3.3 Ma. Exhumation of the blueschist facies sequences was initiated at ca. 54 Ma and involved tectonic activity along blueschist facies and greenschist facies mylonites zones. Final WSW-ward transport of the metamorphic sequence across the structurally lowest, and supposed, autochthonous, series occurred at around 45 Ma, and resulted in termination of the ductile deformation history in the studied area. This study confines the onset of high-pressure metamorphism in the Pelagonian Zone to an interval between 100 Ma and 85 Ma and has shown that high-pressure metamorphism had terminated by ca. 54 Ma. The recognition of an early to middle Alpine cycle, lasting over 30 million years and involving crustal shortening, high-pressure metamorphism, exhumation and subsequent crustal shortening is a key contribution to a better understanding of the early Alpine tectonic history of the Aegean region and eastern Mediterranean." @default.
• W2015496622 created "2016-06-24" @default.
• W2015496622 creator A5007667710 @default.
• W2015496622 creator A5015332862 @default.
• W2015496622 creator A5029549010 @default.
• W2015496622 date "1998-11-01" @default.
• W2015496622 modified "2023-10-16" @default.
• W2015496622 title "40Ar/39Ar laserprobe direct dating of discrete deformational events: a continuous record of early Alpine tectonics in the Pelagonian Zone, NW Aegean area, Greece" @default.
• W2015496622 cites W1967419716 @default.
• W2015496622 cites W1968617532 @default.
• W2015496622 cites W1973726675 @default.
• W2015496622 cites W1975431939 @default.
• W2015496622 cites W1981244912 @default.
• W2015496622 cites W1990336123 @default.
• W2015496622 cites W2005069119 @default.
• W2015496622 cites W2005579073 @default.
• W2015496622 cites W2006724835 @default.
• W2015496622 cites W2009195085 @default.
• W2015496622 cites W2017530353 @default.
• W2015496622 cites W2038507867 @default.
• W2015496622 cites W2039850977 @default.
• W2015496622 cites W2053396954 @default.
• W2015496622 cites W2059380579 @default.
• W2015496622 cites W2060770869 @default.
• W2015496622 cites W2066890973 @default.
• W2015496622 cites W2067124013 @default.
• W2015496622 cites W2072680965 @default.
• W2015496622 cites W2074881770 @default.
• W2015496622 cites W2076580240 @default.
• W2015496622 cites W2077153961 @default.
• W2015496622 cites W2091827040 @default.
• W2015496622 cites W2095053037 @default.
• W2015496622 cites W2100867694 @default.
• W2015496622 cites W2110521620 @default.
• W2015496622 cites W2120619916 @default.
• W2015496622 cites W2165000190 @default.
• W2015496622 cites W2171531907 @default.
• W2015496622 cites W2315614536 @default.
• W2015496622 cites W2319489163 @default.
• W2015496622 cites W2324823344 @default.
• W2015496622 cites W2555797041 @default.
• W2015496622 cites W34252736 @default.
• W2015496622 doi "https://doi.org/10.1016/s0040-1951(98)00181-4" @default.
• W2015496622 hasPublicationYear "1998" @default.
• W2015496622 type Work @default.
• W2015496622 sameAs 2015496622 @default.
• W2015496622 citedByCount "79" @default.
• W2015496622 countsByYear W20154966222012 @default.
• W2015496622 countsByYear W20154966222013 @default.
• W2015496622 countsByYear W20154966222014 @default.
• W2015496622 countsByYear W20154966222015 @default.
• W2015496622 countsByYear W20154966222016 @default.
• W2015496622 countsByYear W20154966222017 @default.
• W2015496622 countsByYear W20154966222018 @default.
• W2015496622 countsByYear W20154966222019 @default.
• W2015496622 countsByYear W20154966222020 @default.
• W2015496622 countsByYear W20154966222021 @default.
• W2015496622 countsByYear W20154966222022 @default.
• W2015496622 countsByYear W20154966222023 @default.
• W2015496622 crossrefType "journal-article" @default.
• W2015496622 hasAuthorship W2015496622A5007667710 @default.
• W2015496622 hasAuthorship W2015496622A5015332862 @default.
• W2015496622 hasAuthorship W2015496622A5029549010 @default.
• W2015496622 hasConcept C109007969 @default.
• W2015496622 hasConcept C12294951 @default.
• W2015496622 hasConcept C127313418 @default.
• W2015496622 hasConcept C127413603 @default.
• W2015496622 hasConcept C140998209 @default.
• W2015496622 hasConcept C146588470 @default.
• W2015496622 hasConcept C147176958 @default.
• W2015496622 hasConcept C151730666 @default.
• W2015496622 hasConcept C160776313 @default.
• W2015496622 hasConcept C173347748 @default.
• W2015496622 hasConcept C17409809 @default.
• W2015496622 hasConcept C195963834 @default.
• W2015496622 hasConcept C197737763 @default.
• W2015496622 hasConcept C23295444 @default.
• W2015496622 hasConcept C26687426 @default.
• W2015496622 hasConcept C2781297371 @default.
• W2015496622 hasConcept C58097730 @default.
• W2015496622 hasConcept C77928131 @default.
• W2015496622 hasConceptScore W2015496622C109007969 @default.
• W2015496622 hasConceptScore W2015496622C12294951 @default.
• W2015496622 hasConceptScore W2015496622C127313418 @default.
• W2015496622 hasConceptScore W2015496622C127413603 @default.
• W2015496622 hasConceptScore W2015496622C140998209 @default.
• W2015496622 hasConceptScore W2015496622C146588470 @default.
• W2015496622 hasConceptScore W2015496622C147176958 @default.
• W2015496622 hasConceptScore W2015496622C151730666 @default.
• W2015496622 hasConceptScore W2015496622C160776313 @default.
• W2015496622 hasConceptScore W2015496622C173347748 @default.
• W2015496622 hasConceptScore W2015496622C17409809 @default.
• W2015496622 hasConceptScore W2015496622C195963834 @default.
• W2015496622 hasConceptScore W2015496622C197737763 @default.
• W2015496622 hasConceptScore W2015496622C23295444 @default.
• W2015496622 hasConceptScore W2015496622C26687426 @default.
• W2015496622 hasConceptScore W2015496622C2781297371 @default.
• W2015496622 hasConceptScore W2015496622C58097730 @default.

• next