Department of Geology, Tarbiat Modares University (TMU), Tehran, 14115-175, Iran
Research Institute for Earth Sciences, Tehran, 13185-1494, Iran
Ian T. Graham
Earth and Sustainability Science Research Centre, School of Biological, Earth and Environmental Sciences, The University of New South Wales, Sydney, NSW 2052, Australia
Mathieu Benoit
Géosciences Environnement Toulouse (GET), Observatoire Midi Pyrénées (OSU-OMP), Université de Toulouse, CNRS, IRD, 14 Avenue E. Belin, Toulouse, 31400, France
Fatemeh Sepidbar
Department of Geology, Faculty of Sciences, Ferdowsi University of Mashhad, Mashhad, Iran
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The vast Cenozoic arc magmatism of Iran introduced three distinct rock series. The LILE (large-ion lithophile elements)-rich and LILE-poor series show signatures of fluid-rich and fluid-poor slab-melt mantle metasomatism, furnished by hot slab subduction. The slab was more hydrated in the northern segment of the study area, where the LILE-rich series dominates. The third series rich in incompatible trace elements, the ITE-rich series, indicates the input of asthenosphere as well.
The vast Cenozoic arc magmatism of Iran introduced three distinct rock series. The LILE...