Abstract
SHRIMP U/Pb age determinations on plagiogranite zircons in the Zone of Bellinzona-Dascio ophiolites yield late Jurassic ages of 149 ± 3 Ma and 142 ± 5 Ma. The plagiogranites are part of a rodingitized and metamorphosed yet well preserved igneous oceanic suite including Mg-gabbros, Fe-Ti-rich gabbros and basalts that is a common feature of the Jurassic Piemont-Ligurian ophiolites. These magmatic ages are among the youngest in this domain and fit well with the observed N-MORB signature of the basalts. The data are indicative of formation in a relatively mature Piemont-Ligurian ocean rather than in an early, embryonic Valaisan ocean.
Original language | English |
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Pages (from-to) | 285-299 |
Number of pages | 15 |
Journal | Schweizerische Mineralogische und Petrographische Mitteilungen |
Volume | 83 |
Issue number | 3 |
Publication status | Published - 2003 |