There are three parallel magmatic arcs in the northwest of Iran, of Cretaceous and Eocene–
Miocene to Quaternary ages, trending in a NW–SE direction between the Main Zagros …

Systematic differences in mineral composition of mantle peridotites are observed in
ophiolites and peridotitic bodies from the Alpine Tethys, the Pyrenean domain, the Dinarides …

There is no consensus on the processes responsible for near-coeval formation of Archaean
continental crust (dominantly tonalite–trondhjemite–granodiorite: TTG), greenstone belts …

Recent geochemical studies of volcanic rocks forming part of the ophiolites within the Zagros
and Naien-Baft orogen indicate that most of them were developed as supra-subduction …

Trace-element compositions of olivine from 75 mantle rocks of diverse origin, including
xenoliths from kimberlites, basaltic lavas and orogenic peridotites, were determined by laser …

Recycled ancient oceanic crust with variable amounts of aging, or inclusion of sediments of
differing types and origins has often been invoked as a source for present‐day ocean island …

Models explaining the characteristic depletion of High Field Strength Elements (HFSE)
relative to elements of similar compatibility in subduction zone magmas invoke either (1) the …

Cenozoic, post-collisional, potassic and ultrapotassic igneous rocks in the North Qiangtang,
Songpan–Ganzi and North Kunlun terranes of the northern Tibetan Plateau are distributed …

Potassic volcanism in the western Sichuan and Yunnan Provinces, SE Tibet, forms part of an
extensive magmatic province in the eastern Indo-Asian collision zone during the Paleogene …

A detailed petrological and geochemical study of low-temperature peridotite xenoliths from
Kimberley and northern Lesotho is presented to constrain the processes that led to the …