Post-emplacement thermo-rheological history of a granite intrusion and surrounding rocks: the Monte Capanne pluton, Elba Island, Italy (Contributo in volume (capitolo o saggio))

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  • Post-emplacement thermo-rheological history of a granite intrusion and surrounding rocks: the Monte Capanne pluton, Elba Island, Italy (Contributo in volume (capitolo o saggio)) (literal)
Anno
  • 2014-01-01T00:00:00+01:00 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
  • 10.1144/SP394.1 (literal)
Alternative label
  • Caggianelli, Alfredo; Ranalli, Giorgio; Lavecchia, Alessio; Liotta, Domenico; Dini, Andrea (2014)
    Post-emplacement thermo-rheological history of a granite intrusion and surrounding rocks: the Monte Capanne pluton, Elba Island, Italy
    The Geological Society of London, London (Regno Unito) in Deformation Structures and Processes within the Continental Crust., 2014
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • Caggianelli, Alfredo; Ranalli, Giorgio; Lavecchia, Alessio; Liotta, Domenico; Dini, Andrea (literal)
Pagina inizio
  • 129 (literal)
Pagina fine
  • 143 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#titoloVolume
  • Deformation Structures and Processes within the Continental Crust. (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#volumeInCollana
  • 394 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#pagineTotali
  • 15 (literal)
Note
  • ISI Web of Science (WOS) (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • University of Bari Carleton University, Ottawa, Canada Istituto di Geoscienze e Georisorse, CNR, Pisa (literal)
Titolo
  • Post-emplacement thermo-rheological history of a granite intrusion and surrounding rocks: the Monte Capanne pluton, Elba Island, Italy (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#curatoriVolume
  • Llana-Funez, S., Marcos, A. & Bastida, F. (literal)
Abstract
  • A thermo-rheological model of the Monte Capanne pluton, Elba Island, Italy is pro- posed as having general relevance for the thermal and tectonic evolution of upper crustal granites and their surrounding rocks in extensional regions. The thermal evolution of the pluton and coun- try rocks is followed for 1 myr after emplacement, which occurred at c. 6.9 Ma. The pluton com- pletely crystallized in c. 210 kyr (+20%). The adjacent rocks reached a thermal peak of 550 8C (+10%), maintaining a temperature higher than 500 8C for c. 100 kyr. The temperature distribution is used to construct a model for the time-dependent rheology of the pluton and surrounding rocks. A series of 2D cross-sections shows an upward migration of the regional brittle 2 ductile transition, and the formation of a ductile horizon above the pluton. The former is a combined effect of unroofing and middle crust heating; the latter is the result of temperature increase in rheologically weak country rocks. This ductile horizon has a potential role in the tectonic evolution of the region, since it could favour the formation of upper crustal shear zones and listric faults rooting in the transient brittle 2 ductile transition and playing a major role in further post-emplacement extension. (literal)
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