Results 101 to 110 of about 1,221,168 (223)

Mesozoic crustal growth and recycling along the Southern margin of Eurasia: magmatic rocks from the Sanandaj-Sirjan Zone of Iran

open access: yes
The Sanandaj-Sirjan Zone of western Iran is characterized by significant Mesozoic magmatic activity (from the early Jurassic to the late Cretaceous), with Cenozoic rocks being less common.
Ghorbani, Ghasem   +12 more
core   +1 more source

Tourmaline chemistry in Malayer-Boroujerd-Shazand, (Sanandaj-Sirjan Zone) [PDF]

open access: yesIranian Journal of Crystallography and Mineralogy, 2019
Kamal Siahcheshm   +3 more
openaire   +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

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

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