دورية أكاديمية
Basement provenance revealed by U-Pb detrital zircon ages: A tale of African and European heritage in Tuscany, Italy
| العنوان: | Basement provenance revealed by U-Pb detrital zircon ages: A tale of African and European heritage in Tuscany, Italy |
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| المؤلفون: | PAOLI, GABRIELE, Stokke, Henrik H., ROCCHI, SERGIO, Sirevaag, Hallgeir, Ksienzyk, Anna K., Jacobs, Joachim, Košler, Jan |
| المساهمون: | Paoli, Gabriele, Stokke, Henrik H., Rocchi, Sergio, Sirevaag, Hallgeir, Ksienzyk, Anna K., Jacobs, Joachim, Košler, Jan |
| سنة النشر: | 2017 |
| المجموعة: | ARPI - Archivio della Ricerca dell'Università di Pisa |
| مصطلحات موضوعية: | Detrital zircon, European terrane, Peri-Gondwana terrane, Provenance, Tuscan basement, U-Pb dating, Geochemistry and Petrology |
| الوصف: | A new data set of ca. 500 LA-ICP-MS U-Pb detrital zircon ages for six metasedimentary units from the Tuscan basement (Apuan Alps, Monti Pisani, Monticiano-Roccastrada), along with a precise SHRIMP U-Pb crystallization age of a metavolcanic unit (Apuan Alps) have been collected to determine their depositional ages and provenance. These results have been integrated with the recently published ca. 900 U-Pb detrital zircon ages from Elba Island to draw a complete picture of the Paleozoic journey of the Tuscan basement. A major change in the sources supplying sediments to the Tuscan basins is shown to occur during this journey. Detrital zircon ages of early Cambrian to middle Ordovician metasediments mirror those of coeval northern Africa sediments: most samples were sourced in western Africa, while one sample is derived material from central northern Africa. The Tuscan block was therefore located at the peri-Gondwana margin, close to central northern Africa. The prominent mid-Ordovician magmatic arc activity (ca. 460. Ma) at the northern Gondwana margin and its detritus, characterise the zircon age distribution of Ordovician and Silurian volcano-sedimentary rocks, that were therefore generated at the northernmost Gondwana margin during subduction and subsequent initial Paleotethys rifting. The Carboniferous-Permian metasediments are dominated by populations of Ordovician and Variscan-age zircons, with a minor occurrence of Neoarchean and Paleoproterozoic zircons that is best explained by recycling of European Neoproterozoic-Cambrian metasediments. In summary, the main sources supplying the Tuscan basins were located in northern Africa throughout Cambrian-Ordovician times, shifting to the volcanic arc active at the northern Gondwana margin during the middle Ordovician. During Variscan and post-Variscan times, detrital zircon sources were mostly located in European terrains, witnessing the shift of Tuscany from Africa to Europe. |
| نوع الوثيقة: | article in journal/newspaper |
| وصف الملف: | STAMPA |
| اللغة: | English |
| ردمك: | 978-0-02-449371-2 0-02-449371-6 |
| العلاقة: | info:eu-repo/semantics/altIdentifier/wos/WOS:000399514500022; volume:277; firstpage:376; lastpage:387; numberofpages:12; journal:LITHOS; http://hdl.handle.net/11568/838543Test; info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-85029560894; https://www.sciencedirect.com/science/article/pii/S0024493716304133Test |
| DOI: | 10.1016/j.lithos.2016.11.017 |
| الإتاحة: | https://doi.org/10.1016/j.lithos.2016.11.017Test http://hdl.handle.net/11568/838543Test https://www.sciencedirect.com/science/article/pii/S0024493716304133Test |
| حقوق: | info:eu-repo/semantics/openAccess |
| رقم الانضمام: | edsbas.B2EF7012 |
| قاعدة البيانات: | BASE |
| ردمك: | 9780024493712 0024493716 |
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| DOI: | 10.1016/j.lithos.2016.11.017 |