Evolution of the Zagros sector of Neo-Tethys: Tectonic and magmatic events that shaped its rifting, seafloor spreading and subduction history
The evolution of the Neo-Tethys realm had a significant impact on the Phanerozoic
paleogeography of the Iran Plateau. However, there remains significant debate regarding …
paleogeography of the Iran Plateau. However, there remains significant debate regarding …
Tethyan subduction and Cretaceous rift magmatism at the southern margin of Eurasia: Evidence for crustal evolution of the South Caspian Basin
The Cretaceous rift magmatic activity along the southern margin of Eurasia is ideal for
testing how the far-field magmatism, with alkaline to calc-alkaline igneous rocks along the …
testing how the far-field magmatism, with alkaline to calc-alkaline igneous rocks along the …
The Sanandaj-Sirjan Zone (W. Iran) was a Jurassic passive continental margin: Evidence from igneous rocks of the Songhor area
It is important to understand the Jurassic tectonic setting of SW Eurasia, and the igneous
rocks of the Sanandaj-Sirjan zone in SW Iran provide critical evidence. Bimodal volcanic …
rocks of the Sanandaj-Sirjan zone in SW Iran provide critical evidence. Bimodal volcanic …
A Jurassic volcanic passive margin in Iran and Turkey
Abstract Broadly similar Early to Middle Jurassic stratigraphic sequences including bimodal
igneous rocks of the Sanandaj–Sirjan Zone of Iran and the Sakarya Zone of Turkey suggest …
igneous rocks of the Sanandaj–Sirjan Zone of Iran and the Sakarya Zone of Turkey suggest …
S-type like granites and felsic volcanic rocks in the Mahabad area, NW Iran: Late Neoproterozoic extensional tectonics follow collision on the northern boundary of …
Abstract The Late Neoproterozoic basement is exposed in the Mahabad area of northwest
Iran, and it is classified into three main groups. The first is metamorphic rocks that include …
Iran, and it is classified into three main groups. The first is metamorphic rocks that include …
Hydrothermal alteration mapping using ASTER data, Takab-Baneh area, NW Iran: A key for further exploration of polymetal deposits
A large number of polymetallic deposits exist in the Takab-Baneh area, NW Iran. Different
methods such as minimum noise fraction (MNF), pixel purity index (PPI), nD visualization …
methods such as minimum noise fraction (MNF), pixel purity index (PPI), nD visualization …
Late Cretaceous-Paleocene Arc and Back-Arc System in the Neotethys Ocean, Zagros Suture Zone
The Bulfat Igneous Complex comprises the Bulfat and Walash groups and is situated in the
Zagros Suture Zone, in the junction of Arabian and Eurasian plates. Zircon U-Pb data indicat …
Zagros Suture Zone, in the junction of Arabian and Eurasian plates. Zircon U-Pb data indicat …
A unique period of bimodal volcanism at 130–110 Ma in the northern Sanandaj-Sirjan Zone: Evidence for an extensional setting
Abstract The Sanandaj-Sirjan metamorphic-magmatic Zone (SaSZ) represents the Mesozoic
active continental margin of the Neotethys Ocean between the Arabian plate and the Iranian …
active continental margin of the Neotethys Ocean between the Arabian plate and the Iranian …
Early Miocene post-collision andesite in the Takab Area, NW Iran
H Azizi, N Daneshvar, A Mohammadi… - Journal of …, 2021 - academic.oup.com
Miocene magmatic rocks are exposed as lava flows (OKV group), subvolcanic rocks (SRG
group), and as lavas interbedded with shallow-basin sedimentary layers (TVN group) in the …
group), and as lavas interbedded with shallow-basin sedimentary layers (TVN group) in the …
From Early Jurassic intracontinental subduction to Early-Middle Jurassic slab break-off magmatism during the Cimmerian orogeny in the Sanandaj-Sirjan Zone, Iran
N Shabanian, F Neubauer - Journal of Asian Earth Sciences, 2024 - Elsevier
This study aims to review the Jurassic to Cretaceous tectonic setting of the Sanandaj-Sirjan
Zone (SaSZ), the inner part of the Zagros orogen. For many years, the SaSZ was interpreted …
Zone (SaSZ), the inner part of the Zagros orogen. For many years, the SaSZ was interpreted …