Geochemical and Sr–Nd–Hf isotopic evidence for Cenozoic partial melting of mantle beneath Natanz, Central Iran

Geochemical and Sr–Nd–Hf isotopic evidence for Cenozoic partial melting of mantle beneath Natanz, Central Iran

The products of Cenozoic continental arc magmatism in Iran provide an outstanding natural laboratory for investigating subduction-related processes. Here we present whole rock, Sr[sbnd]Nd isotopic, zircon U–Pb–Hf age, and mineral composition data for Cenozoic intrusive rocks from the Natanz area, ce...

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Bibliographic Details
Main Authors:	Babazadeh, S, D'Antonio, M, Raeisi, D, Furman, T, Santosh, M, Di Renzo, V, Klötzli, U, Choi, SH, Ghalamghash, J, Cottle, JM, Palin, R
Format:	Journal article
Language:	English
Published:	Elsevier 2024

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