Crustal anatexis is an important process in the tectonic evolution of many orogenic systems.
In the Wuyi-Yunkai orogen in the South China block, the duration of partial melting and its …

This work investigates the petrogenesis of the main magmatic rocks of the Jurassic Alvand
plutonic complex, located in the northern sector of the Sanandaj-Sirjan Zone of Iran. The …

Meta-pelitic rocks with interlayers of meta-psammites within the inner thermal aureole of the
Alvand plutonic complex (Sanandaj-Sirjan Zone (SaSZ), western Iran) underwent partial …

The Hamadan high-grade metapelites in the northwestern part of the Sanandaj–Sirjan zone,
Iran, show a polymetamorphic evolution with relics of a garnet-bearing metamorphic mineral …

This work describes the petrogenesis of in situ and in-source trondhjemite leucosomes
generated by low-degree partial melting of the Jurassic Cheshmeh-Ghasaban hornblende …

Amphibole-dominated dehydration melting of gabbro is the primary process responsible for
the genesis of adakites, low-K tonalites, modern trondhjemites, and plagiogranites as well …

Abstract Subduction of Neo-Tethys oceanic lithosphere beneath the Iranian plate during the
Mesozoic formed several igneous bodies of ultramafic to intermediate and felsic …

Pegmatite bodies with a simple mineral composition are widespread within the Sanandaj-
Sirjan Zone (SaSiZ), Zagros Orogen, Iran; however, gem-bearing pegmatite bodies are rare …

The study area is a part of the NW to SE strik ing Sanandaj–Sirjan meta mor phic belt in west
ern Iran. The Alvand Pluton, consist ing of rocks that range in com po si tion from gab bro to …

Migmatites record crucial information about the rheology and tectonothermal evolutionof the
deep crust during orogenesis. In the Wuyi–Yunkai orogen in South China, migmatites at …