http://www.cnr.it/ontology/cnr/individuo/prodotto/ID29448
Petrology and 40Ar39Ar dating of shear zones in the Lanterman Range (northern Victoria Land, Antarctica): implications for metamorphic and temporal evolution at the terrane boundaries. (Articolo in rivista)
- Type
- Label
- Petrology and 40Ar39Ar dating of shear zones in the Lanterman Range (northern Victoria Land, Antarctica): implications for metamorphic and temporal evolution at the terrane boundaries. (Articolo in rivista) (literal)
- Anno
- 2007-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1007/s00710-006-0164-2 (literal)
- Alternative label
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Crispini L.; Di Vincenzo G.; Palmeri R. (literal)
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- http://www.springerlink.com/content/1438-1168/ (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Rivista
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#note
- DOI 10.1007/s00710-006-0164-2. (literal)
- Note
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- Dipartimento per lo studio del Territorio e delle sue Risorse, Universit?à di Genova, Genova, Italy;
Istituto di Geoscienze e Georisorse - CNR, Pisa, Italy;
Museo Nazionale dell'Antartide, Università di Siena, Siena, Italy (literal)
- Titolo
- Petrology and 40Ar39Ar dating of shear zones in the Lanterman Range (northern Victoria Land, Antarctica): implications for metamorphic and temporal evolution at the terrane boundaries. (literal)
- Abstract
- The Lanterman Fault Zone, a major terrane boundary in northern Victoria Land, displays a polyphase structural evolution. After west-over-east thrusting, it experienced sinistral strike-slip shearing. Sheared metabasites from the Wilson Terrane (inboard terrane) preserve a record of retrograde metamorphic evolution. Shearing took place under amphibolite-facies metamorphic conditions (roughly comparable to those reached during regional metamorphism) which later evolved to greenschist-facies conditions. In contrast, the Bowers Terrane (outboard terrane) preserves a prograde metamorphic evolution which developed from greenschist-facies to amphibolite-facies metamorphism during shearing, followed by greenschist-facies metamorphism during the late deformational stages. Laser step-heating 40Ar-39Ar analyses of syn-shear amphibolite-facies amphiboles yielded ages of 480-460 Ma, in agreement with a ?480-Ma age obtained from a biotite aligned along the mylonitic foliation. These ages are younger than those (?492 to ?495 Ma) obtained from pre-shear amphibole relics linked to regional metamorphism of the Wilson Terrane. Results attribute the structural
and metamorphic reworking during shearing to the late stages of the Cambrian-Ordovician Ross Orogeny and to the Middle-Late Ordovician probably in relation to the beginning of deformation in the Lachlan Orogen, thus precluding any appreciable impact of the Devonian-Carboniferous Borchgrevink event in the study area. (literal)
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