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 …
Fate of an oceanic plate in the Neo-Tethys intra-oceanic subduction system: Evidence from elemental and Rb/Sr–Sm/Nd isotopic systematics
We report the coexistence of normal mid-ocean ridge basalt (NMORB)-type and alkaline
ocean island basalt (OIB)-type mafic volcanics from the Zildat Ophiolitic Mélange (ZOM) …
ocean island basalt (OIB)-type mafic volcanics from the Zildat Ophiolitic Mélange (ZOM) …
Long-lived, Eocene-Miocene stationary magmatism in NW Iran along a transform plate boundary
Abstract The Eocene-Miocene Mianeh-Hashtroud igneous district in NW Iran is part of the
Turkish–Caucasus–Iranian collision zone, a key region to decipher the assembly and …
Turkish–Caucasus–Iranian collision zone, a key region to decipher the assembly and …
The Van microplate: a new microcontinent at the junction of Iran, Turkey, and Armenia
In northwestern Iran, magmatic activity occurred during three main intervals: The
Cretaceous, Eocene, and Miocene-Quaternary. The first two phases of magmatic activity are …
Cretaceous, Eocene, and Miocene-Quaternary. The first two phases of magmatic activity are …
Continental crust variance between post-collisional compressional and extensional domains controlled magmatic activity at Damavand volcano, Northern Iran
H Azizi, F Nouri, Y Asahara, M Minami… - International Geology …, 2024 - Taylor & Francis
ABSTRACT The Quaternary Damavand stratovolcano, with an elevation of 5670 m, is the
highest mountain in Iran and is the subject of this study. The main rocks are trachyandesite …
highest mountain in Iran and is the subject of this study. The main rocks are trachyandesite …
Geochemistry and petrogenesis of ophiolitic rocks from the Indus Suture Zone (ISZ), Ladakh Himalaya: insights for depleted mantle beneath an intra-oceanic island …
ABSTRACT The Indus Suture Zone preserves the ophiolitic remnants of the eastern part of
the Neo-Tethys Ocean. Parts of these ophiolitic remnants are exposed along the Khangral …
the Neo-Tethys Ocean. Parts of these ophiolitic remnants are exposed along the Khangral …
The Paleogene ophiolite conundrum of the Iran–Iraq border region
New and compiled geochemical, isotopic and geochronological data allow us to propose a
new explanation for Paleogene oceanic magmatic rocks along the Iran–Iraq border. These …
new explanation for Paleogene oceanic magmatic rocks along the Iran–Iraq border. These …
Petrology and geochemistry of mafic intrusive rocks from the Sapi-Shergol ophiolitic mélange, Indus Suture Zone, western Ladakh: constraints on petrogenesis and …
This article reports the existence of subduction-related tholeiitic, normal mid-ocean ridge
basalt (N-MORB)-type mafic intrusives emplaced within the Sapi-Shergol ophiolitic mélange …
basalt (N-MORB)-type mafic intrusives emplaced within the Sapi-Shergol ophiolitic mélange …
[HTML][HTML] Petrology of the Paleogene shoshonitic volcanism in north Sarab area, NW Iran: Geochemical, Ar-Ar dating and Sr-Nd-Pb isotopic constraints
S Heidari, AAT Shabani, S Hassanpour… - Journal of Asian Earth …, 2022 - Elsevier
This study reports the earliest presumably known collisional magmatism of the NW Iran–
eastern Turkey–Caucasus region from the north of Sarab city in East Azarbaijan province …
eastern Turkey–Caucasus region from the north of Sarab city in East Azarbaijan province …
Geochronology, petrogenesis, and tectonic setting of amphibolitic rocks from the Tutak metamorphic Complex, Sanandaj-Sirjan Zone, Iran
E Moradian, N Shabanian, AR Davoudian… - Journal of Asian Earth …, 2023 - Elsevier
Amphibolitic rocks of the Tutak Metamorphic Complex (TMC), in the southern part of the
Sanandaj Sirjan Zone (SaSZ), are associated with meta-dolerites, felsic intrusions, mica …
Sanandaj Sirjan Zone (SaSZ), are associated with meta-dolerites, felsic intrusions, mica …