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A Sm-Nd isotopic study of 500 Ma old oceanic crust in the Variscan belt of Western Europe: the Chamrousse ophiolite complex, Western Alps (France)

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Abstract

We report the results of a Sm-Nd isotopic study of whole-rock samples from the Chamrousse ophiolite complex, in the Variscan basement of the Western Alps, France. Our data point to a 497±24 (2σ) Ma age, in excellent agreement with U-Pb results (Ménot et al. 1984) on subordinate plagiogranites. Strong isotopic heterogeneity and time evolution of magmas from relatively less depleted (ɛ Nd= +5) to very depleted (ɛ Nd= +9) sources are also implied. Available data favour a mixing model between N-MORB and E-MORB type end-members, but a third component with distinct “supra-subduction zone” affinity is also required. These results preclude any tectonic setting such as intracontinental rift, ensialic marginal basin, or major ocean ridge, but substantiate an oceanic back-arc environment. They also demonstrate that the well-documented Upper Cambrian-Lower Ordovician extensional phase here reached a true oceanic stage.

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Pin, C., Carme, F. A Sm-Nd isotopic study of 500 Ma old oceanic crust in the Variscan belt of Western Europe: the Chamrousse ophiolite complex, Western Alps (France). Contr. Mineral. and Petrol. 96, 406–413 (1987). https://doi.org/10.1007/BF00371258

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