Williams, Ian; Fiannacca, Patrizia; Cirrincione, Rosolino; Pezzino, Antonino
The ages of detrital zircon grains from one paragneiss and inherited zircon cores from two augen gneisses from the amphibolite facies basement of the Peloritani Mountains (southern Italy) measured by SHRIMP U-Pb constrain the previously unknown deposition age of the original sediments and help to elaborate a model for their provenance and subsequent evolution. The deposition age is latest Neoproterozoic to Cambrian (~ 545. Ma), bracketed by the combined ages of the youngest detrital/inherited...[Show more]
Items in Open Research are protected by copyright, with all rights reserved, unless otherwise indicated.