International audienceThe Urumieh plutonic complex is located in the northwestern part of the Sanandaj–Sirjan zone (Iran). The Urumieh plutonic complex comprises three components, i.e.
Vosoughi-Abedinic, M. +4 more
core +1 more source
Metamorphism at convergent plate margins: Preface. [PDF]
Palin RM, Roberts NMW.
europepmc +1 more source
Relationship between deformation structure and partial melting in pelitic migmatites of Hamaden region, Sanandaj-Sirjan Zone [PDF]
The present paper describes some field characteristics of deformation in a high-strain and high temperature zone in migmatitic rocks, with several kilometers wide occurring in Hamedan and Toyserkan regions, NW of the Sanandaj- Sirjan Zone.
Leyli Izadi Kian, Seyedeh Razieh Jafari
core +2 more sources
The tectonic setting in which Jurassic igneous rocks of the Sanandaj-Sirjan Zone (SaSZ) of Iran formed is controversial. SaSZ igneous rocks are mainly intrusive granodiorite to gabbroic bodies, which intrude Early to Middle Jurassic metamorphic basement;
Hasannejad S. +4 more
core +1 more source
Groundwater sustainability assessment based on socio-economic and environmental variables: a simple dynamic indicator-based approach. [PDF]
Karimi D +4 more
europepmc +1 more source
Early Miocene larger benthic foraminifera from the northwestern Tethyan Seaway (NW Iran): new findings on Shallow Benthic Zone 25. [PDF]
Yazdi-Moghadam M +4 more
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A petrofabric study of deformation in the southeastern Sanandaj-Sirjan metamorphic zone: Constraints from structures and microstructures [PDF]
This study investigates deformation in the Chai-Kour metamorphic complex, located in the Sanandaj-Sirjan metamorphic belt, using structural, microstructural, and strain analyses.
Saeede Keshavarz
doaj
A Robust Deep-Learning Model for Landslide Susceptibility Mapping: A Case Study of Kurdistan Province, Iran. [PDF]
Ghasemian B +8 more
europepmc +1 more source
A recovered Moho model by integrated inversion of gravity and seismic depths in Iran. [PDF]
Ebadi S +3 more
europepmc +1 more source
Ongoing formation of felsic lower crustal channel by relamination in Zagros collision zone revealed from regional tomography. [PDF]
Talebi A +4 more
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