Results 91 to 100 of about 1,166,788 (193)

Geochemistry, Sr-Nd isotope data and petrogenesis of the Marziyan granitoid, Sanandaj-Sirjan Zone, western Iran

open access: yes, 2015
The Marziyan granitoid is part of the widespread granitoid bodies in the Sanandaj-Sirjan Zone. It intruded Mesozoic regional metamorphic rocks of this belt and is composed of leucogranite and subordinate granite.
Datvishi, E.   +5 more
core   +1 more source

The ammonium content in the Malayer igneous and metamorphic rocks (Sanandaj-Sirjan Zone, Western Iran)

open access: yes, 2011
The ammonium content in the Malayer igneous and metamorphic rocks (Sanandaj-Sirjan Zone, Western Iran)The ammonium (NH4+) contents of the Malayer area (Western Iran) have been determined by using the colorimetric method on 26 samples from igneous and ...
Ann Hirt   +3 more
core   +1 more source

Geochemistry and mineral chemistry of Shahabad gabbroic intrusion, NW Nourabad, Lorestan province

open access: yesJournal of Economic Geology, 2013
The Shahabad gabbroic intrusion, with NW-SE trend cropped out at the boundary of Zagros and Sanandaj-Sirjan zones is composed of olivine gabbro, orthogabbro and troctolite.
Reza Zarei Sahamieh   +3 more
doaj  

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

open access: yesHeliyon, 2023
Kianoush P   +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)

open access: yes
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   +4 more
core   +1 more source

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

open access: yesSci Rep, 2021
Kaviani A   +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

open access: yes, 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.   +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

open access: yes, 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   +7 more
core   +1 more source

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