[HTML][HTML] Tectonic, magmatic, and metallogenic evolution of the Tethyan orogen: From subduction to collision
JP Richards - Ore Geology Reviews, 2015 - Elsevier
This paper reviews the tectonic, magmatic, and metallogenic history of the Tethyan orogen
from the Carpathians to Indochina. Focus is placed on the formation of porphyry Cu±Mo±Au …
from the Carpathians to Indochina. Focus is placed on the formation of porphyry Cu±Mo±Au …
Building the Zagros collisional orogen: timing, strain distribution and the dynamics of Arabia/Eurasia plate convergence
The Zagros Mountains are the result of the Arabia/Eurasia collision initiated at~ 35Ma as the
rifted Arabian lithosphere was underthrusted beneath the Iranian plate due to its negative …
rifted Arabian lithosphere was underthrusted beneath the Iranian plate due to its negative …
Zircon U–Pb age constraints from Iran on the magmatic evolution related to Neotethyan subduction and Zagros orogeny
This study reports zircon LA-ICPMS U–Pb ages of 50 igneous rock samples from the
Urumieh–Dokhtar magmatic arc (UDMA) and Sanandaj–Sirjan structural zone (SSZ) in Iran …
Urumieh–Dokhtar magmatic arc (UDMA) and Sanandaj–Sirjan structural zone (SSZ) in Iran …
[HTML][HTML] Temporal–spatial distribution and tectonic setting of porphyry copper deposits in Iran: constraints from zircon U–Pb and molybdenite Re–Os geochronology
M Aghazadeh, Z Hou, Z Badrzadeh, L Zhou - Ore geology reviews, 2015 - Elsevier
Porphyry copper deposits (PCDs) in Iran are dominantly distributed in Arasbaran (NW Iran),
the middle segment of the Urumieh–Dokhtar Magmatic Arc (UDMA), and Kerman (central SE …
the middle segment of the Urumieh–Dokhtar Magmatic Arc (UDMA), and Kerman (central SE …
Eocene–Oligocene post-collisional magmatism in the Lut–Sistan region, eastern Iran: Magma genesis and tectonic implications
Abstract New 40 Ar/39 Ar, geochemical and Srsingle bond Nd isotopic analyses of Eocene–
Oligocene magmatic rocks in the Lut–Sistan region, eastern Iran shed light on their origin …
Oligocene magmatic rocks in the Lut–Sistan region, eastern Iran shed light on their origin …
Late Eocene–Oligocene post-collisional monzonitic intrusions from the Alborz magmatic belt, NW Iran. An example of monzonite magma generation from a …
A potassic magmatic association in the Zagros hinterland of the Tethyan orogen in Iran is
identified and characterized for relevant geochronologic and petrologic features. New data …
identified and characterized for relevant geochronologic and petrologic features. New data …
Long-lived, stationary magmatism and pulsed porphyry systems during Tethyan subduction to post-collision evolution in the southernmost Lesser Caucasus, Armenia …
Abstract The composite Meghri–Ordubad and Bargushat plutons of the Zangezur–Ordubad
region in the southernmost Lesser Caucasus consist of successive Eocene to Pliocene …
region in the southernmost Lesser Caucasus consist of successive Eocene to Pliocene …
Cenozoic porphyry and other hydrothermal ore deposits along the South Caucasus-West Iranian tectono-magmatic belt: a critical reappraisal of the controlling factors
In this contribution, we investigate the space and time distribution of the Cenozoic
magmatism and the associated porphyry Cu-Mo±Au and other hydrothermal (mostly …
magmatism and the associated porphyry Cu-Mo±Au and other hydrothermal (mostly …
Mineral assemblages, fluid evolution, and genesis of polymetallic epithermal veins, Glojeh district, NW Iran
The Glojeh district contains silver-and base metal-rich epithermal veins and is one of the
most highly mineralized locations in the Tarom-Hashtjin metallogenic province …
most highly mineralized locations in the Tarom-Hashtjin metallogenic province …
Petrogenesis of Tarom high-potassic granitoids in the Alborz–Azarbaijan belt, Iran: Geochemical, U–Pb zircon and Sr–Nd–Pb isotopic constraints
Abstract Large-scale Upper Eocene plutons in the Western Alborz–Azarbaijan orogenic belt
mostly show calc-alkaline and I-type geochemical features contrasted by the Tarom complex …
mostly show calc-alkaline and I-type geochemical features contrasted by the Tarom complex …