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| Content Provider | Springer Nature Link |
|---|---|
| Author | Lotout, Caroline Pitra, Pavel Poujol, Marc Den Driessche, Jean |
| Copyright Year | 2016 |
| Abstract | New U–Pb dating on zircon yielded ca. 470 Ma ages for the granitoids from the Lévézou massif in the southern French Massif Central. These new ages do not support the previous interpretation of these granitoids as syn-tectonic intrusions emplaced during the Late Devonian-Early Carboniferous thrusting. The geochemical and isotopic nature of this magmatism is linked to a major magmatic Ordovician event recorded throughout the European Variscan belt and related to extreme thinning of continental margins during a rifting event or a back-arc extension. The comparable isotopic signatures of these granitoids on each side of the eclogite-bearing leptyno-amphibolitic complex in the Lévézou massif, together with the fact that they were emplaced at the same time, strongly suggest that these granitoids were originally part of a single unit, tectonically duplicated by either isoclinal folding or thrusting during the Variscan tectonics. |
| Starting Page | 501 |
| Ending Page | 515 |
| Page Count | 15 |
| File Format | |
| ISSN | 14373254 |
| Journal | International Journal of Earth Sciences |
| Volume Number | 106 |
| Issue Number | 2 |
| e-ISSN | 14373262 |
| Language | English |
| Publisher | Springer Berlin Heidelberg |
| Publisher Date | 2016-08-13 |
| Publisher Place | Berlin, Heidelberg |
| Access Restriction | One Nation One Subscription (ONOS) |
| Subject Keyword | Variscan Orthogneiss Geochronology U/Pb Ordovician Geochemistry Geology Geophysics/Geodesy Sedimentology Structural Geology Mineral Resources |
| Content Type | Text |
| Resource Type | Article |
| Subject | Earth and Planetary Sciences |
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