Poly-Orogenic Melting of Metasedimentary Crust From a Granite Geochemistry and Inherited Zircon Perspective (Southern Calabria-Peloritani Orogen, Italy)

Inherited zircon ages and geochemical features of late Cadomian and late Variscan granitoids from the north-eastern Peloritani Mountains (NE Sicily) and the western Aspromonte Massif (SW Calabria) shed new light on the sources and processes involved in poly-orogenic granitoid magmatism. The two grou...

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Autori principali: Patrizia Fiannacca, Ian S. Williams, Rosolino Cirrincione, Antonino Pezzino
Natura: Artigo
Lingua:Inglês
Pubblicazione: Frontiers Media S.A. 2019-05-01
Serie:Frontiers in Earth Science
Soggetti:
S-type granites
meta-greywackes
zircon inheritance
whole rock chemistry
crustal melting
Cadomian
Accesso online:https://www.frontiersin.org/article/10.3389/feart.2019.00119/full
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