The geodynamic evolution of Iran
Iran is a remarkable geoscientific laboratory where the full range of processes that form and
modify the continental crust can be studied. Iran's crustal nucleus formed as a magmatic arc …
modify the continental crust can be studied. Iran's crustal nucleus formed as a magmatic arc …
The North Sistan orogen (Eastern Iran): Tectono-metamorphic evolution and significance within the Tethyan realm
Abstract The Sistan orogen (Eastern Iran) separates the Afghan and Lut continental blocks
and stretches along∼ 700 km from north to south, at a high angle with respect to other …
and stretches along∼ 700 km from north to south, at a high angle with respect to other …
The Middle Jurassic Cheshmeh-Ghasaban High-Mg gabbro (Hamedan, NW Iran): A plume-influenced intracontinental rifting event?
The Jurassic mafic to felsic magmatism affecting the older Ediacaran-to-Cambrian basement
of the Sanandaj-Sirjan Zone of Iran has been traditionally interpreted as the product of arc …
of the Sanandaj-Sirjan Zone of Iran has been traditionally interpreted as the product of arc …
New evidence for Late Cretaceous plume-related seamounts in the Middle East sector of the Neo-Tethys: Constraints from geochemistry, petrology, and mineral …
Abstract The Durkan Complex in the Makran Accretionary Prism (SE Iran) has been
interpreted either as a continental margin succession or a Late Cretaceous tectonically …
interpreted either as a continental margin succession or a Late Cretaceous tectonically …
Gold and sulfide-bearing listvenite in the mantle section of the Tays ophiolite in the Arabian Shield, Saudi Arabia
The mantle section of the Late Neoproterozoic Tays ophiolite in the Arabian Shield consists
principally of thoroughly serpentinized peridotite with characteristics typical of depleted …
principally of thoroughly serpentinized peridotite with characteristics typical of depleted …
A resource for automated search and collation of geochemical datasets from journal supplements
This article presents a resource for automated search, extraction and collation of
geochemical and geochronological data from the Figshare repository using web scraping …
geochemical and geochronological data from the Figshare repository using web scraping …
[HTML][HTML] The western Durkan Complex (Makran Accretionary Prism, SE Iran): A Late Cretaceous tectonically disrupted seamounts chain and its role in controlling …
Abstract The Durkan Complex is a key tectonic element of the Makran accretionary prism
(SE Iran) and it has been interpreted as representing a continental margin succession. We …
(SE Iran) and it has been interpreted as representing a continental margin succession. We …
Unravelling metamorphic ages of suture zone rocks from the Sabzevar and Makran areas (Iran): Robust age constraints for the larger Arabia–Eurasian collision zone
In this study we establish a time frame for metamorphic processes affecting Neotethyan
suture zones at the northern (Sabzevar) and southern (Makran) margin of the Central Iranian …
suture zones at the northern (Sabzevar) and southern (Makran) margin of the Central Iranian …
[HTML][HTML] Geochemistry of volcanic rocks and dykes from the Remeshk-Mokhtarabad and Fannuj-Maskutan Ophiolites (Makran Accretionary Prism, SE Iran): new …
Abstract The Remeshk-Mokhtarabad and Fannuj-Maskutan ophiolites represent two major
ophiolitic units in the North Makran Domain (Makran Accretionary Prism). Volcanic rocks and …
ophiolitic units in the North Makran Domain (Makran Accretionary Prism). Volcanic rocks and …
The Bajgan Complex revealed as a Cretaceous ophiolite-bearing subduction complex: A key to unravel the geodynamics of Makran (southeast Iran)
In the Makran area, a wide accretionary wedge is originated by the north-dipping subduction
of the Neo-Tethyan oceanic lithosphere. The rear of the accretionary wedge is represented …
of the Neo-Tethyan oceanic lithosphere. The rear of the accretionary wedge is represented …