Results 101 to 110 of about 1,166,788 (193)

Geobody estimation by Bhattacharyya method utilizing nonlinear inverse modeling of magnetic data in Baba-Ali iron deposit, NW Iran. [PDF]

Heliyon, 2023
Kianoush P, Keshavarz Faraj Khah N, Hosseini SA, Jamshidi E, Afzal P, Ebrahimabadi A.   +5 more
europepmc   +1 more source

Geochemical and Isotopic Constraints on the Origin of the Early Palaeozoic Chah‐Nar Pb–Zn Deposit, Sanandaj–Sirjan Zone (Iran)

The Chah‐Nar Pb–Zn deposit in the southern Sanandaj–Sirjan Zone, Iran, represents Early Palaeozoic stratiform sulfide mineralization hosted by organic‐rich volcano‐sedimentary rocks deposited in a Proto‐Tethyan back‐arc basin.
Matthew I. Leybourne, Sajjad Maghfouri, Mohammad Jafar Kupayi, Hemayat Jamali, Ebrahim Rastad   +4 more
core   +1 more source

Mantle-flow diversion beneath the Iranian plateau induced by Zagros' lithospheric keel. [PDF]

Sci Rep, 2021
Kaviani A, Mahmoodabadi M, Rümpker G, Pilia S, Tatar M, Nilfouroushan F, Yamini-Fard F, Moradi A, Ali MY.   +8 more
europepmc   +1 more source

Jurassic igneous rocks of the central Sanandaj–Sirjan zone (Iran) mark a propagating continental rift, not a magmatic arc

, 2019
Due to copyright restrictions and/or publisher's policy full text access from Treasures at UT Dallas is limited to current UTD affiliates (use the provided Link to Article).Supplementary material is available on publisher's website.
Azizi, H., Robert J. Stern, Stern, Robert J., Hossein Azizi   +3 more
core   +1 more source

An investigation into the fault patterns in the Chadegan region, Iran: evidence for dextral brittle transpressional tectonics in the Sanandaj-Sirjan Zone

, 2012
The NW–SE trending Sanandaj–Sirjan Zone (SSZ) is the internal part of the Zagros continental collision zone, which mainly consists of metamorphic rocks deformed in a dextral transpressional zone.
Davoudian, Ali Reza, Mohammad Mohajjel, Babaahmadi, Abbas, Ali Reza Davoudian, Abbas Eftekhari, Mohajjel, Mohammad, Eftekhari, Abbas, Abbas Babaahmadi   +7 more
core   +1 more source

Appraising Mahallat Geothermal Region using thermal surveying data accompanied by the geological, geochemical and gravity analyses. [PDF]

Sci Rep, 2021
Nouraliee J, Ebrahimi D, Dashti A, Gholami Korzani M, Sangin S.   +4 more
europepmc   +1 more source

The Urumieh plutonic complex (NW Iran): A record of the geodynamic evolution of the Sanandaj–Sirjan zone during Cretaceous times – Part I: Petrogenesis and K/Ar dating

, 2009
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., Bouchez, J. L., Ghalamghash, J., Bellon, H., Nédélec, A.   +4 more
core   +1 more source

Metamorphism at convergent plate margins: Preface. [PDF]

Geosci Front, 2022
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 Late Jurassic Panjeh submarine volcano in the northern Sanandaj-Sirjan Zone, northwest Iran: Mantle plume or active margin?

, 2018
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., Asahara Y., Stern R. J., Lucci F., Azizi H.   +4 more
core   +1 more source