Results 71 to 80 of about 1,166,788 (193)
Metamorphic rocks of the Sanandaj-Sirjan zone host the Muteh gold mining district. The gold occurrences are in northwest-striking and northeast-dipping normal faults crosscutting the regional ductile pattern of the host rocks.
Moritz, Robert, Ghazban, Fereydoun
core +1 more source
Abstract The Zagros orogen records the closure of the Neotethys Ocean by northward subduction of the oceanic slab beneath the Iranian plate. Northwestern Iran has undergone episodic volcanism since the Eocene, due to a shift of tectonic regimes from subduction to collision and post‐collisional extension, although the dynamics responsible for such ...
Farzaneh Shakerardakani +5 more
wiley +1 more source
Introduction The Iranian plateau is part of the Alpine-Himalayan orogenic belt, which consists of several continental fragments separated from each other by major boundary faults and/or ophiolitic suture zones (Gansser, 1981).
Farid Abdollahi +4 more
doaj +1 more source
Abstract The key factor that controls the genesis of porphyry Cu deposits (PCDs) in collisional orogens remains a debated topic. This study employs whole‐rock La/Yb proxies to quantitatively constrain the spatial and temporal variations in crustal thickness of the South Armenian–Iranian magmatic belt (SAIMB) within the Zagros orogen (central Tethys ...
Xuhui WANG +4 more
wiley +1 more source
Carbinatitic magmatism evidence in the Quaternary volcanic rocks in the west of Nowbaran, NW of Iran [PDF]
The fourteen numbers of ultrabasic volcanoes eruption in the west of Nowbaran are located in the west margin of Iranian central zone near to the Sanandaj-Sirjan zone.
Bahman Rahimzadeh +3 more
doaj +1 more source
Mikrofazies, Biostratigraphie und Ablagerungsräume der eozänen Schichtenfolge des Zagros-Gebirges und der Sanandaj-Sirjan-Zone (Iran) [PDF]
Two Eocene sections in the Zagros Mountains and two in Sanandaj-Sirjan Zone of west and cental Iran have been investigated with the purpose to determine the age of the sections based on planktonic and benthic foraminifera, to analyze the sedimentary ...
Almasinia, Banafsheh
core
A total of 41,342 detrital zircon U–Pb ages and 6,129 Hf isotopes were compiled. Different zircon features in response to the tectonic events in the Middle East. Potential uses in provenance and palaeogeographic analysis. Abstract The detrital zircon records significant information in the ‘source‐sink’ system.
Gaoyuan Sun, Jianuo Chen
wiley +1 more source
Geochemistry, mineral chemistry and P-T evaluation of metasediments of Bahram-Gur complex, ES Sanandaj-Sirjan zone, Iran [PDF]
The Bahram-Gur area in the southeastern part of the Sanandaj–Sirjan metamorphic zone, contains metabasites and metasediments. The metasedimentary rocks are mainly garnet schists and garnet-staurolite schists that were metamorphosed under amphibolite ...
Nakashima, Kazu +2 more
core +1 more source
The present study aims to investigate the environmental geochemistry of potentially toxic elements (PTEs) in tailing samples of the Ahangaran Pb-Zn mine, located 95 km southeast of Hamadan.
Mahrokh Ghanbari Mohazzab +2 more
doaj +1 more source
Mineral chemistry and geothermobarometry of gabbroic dykes of the Garmab Ophiolite sequence (Northeast of Kamyaran) [PDF]
The Garmab ophiolite complex, a part of the Ophiolite-Radiolithic zone of Kermanshah, is located in the northeast of Kamyaran. In view of the Iranian geo-structural zones, this complex is situated between the Sanandaj-Sirjan Zone and the Zagros thrust ...
shahryar Mahmoudi +2 more
doaj +1 more source

