Rhenium-osmium isotope and elemental behaviour during subduction of oceanic crust and the implications for mantle recycling

This study presents major-, trace-element, and rhenium-osmium (Re-Os) isotope and elemental data for basalts and gabbros from the Zermatt-Saas ophiolite, metamorphosed to eclogite-facies conditions during the Alpine orogeny. Igneous crystallisation of the gabbros occurred at 163.5 ± 1.8 Ma and both...

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Bibliografski detalji
Glavni autori: Dale, C, Gannoun, A, Burton, K, Argles, T, Parkinson, I
Format: Journal article
Izdano: 2007