Výsledky vyhledávání - "Asghar Dolati"

Akademický článek

nPetrography, geochemistry, and tectonomagmatic model of igneous masses in Gorgan Schist of the south of Behshahr, east of Mazandaran

Autor: sina moradhosseini, shahryar Mahmoudi, Asghar Dolati

Publikováno v: پترولوژی, Vol 13, Iss 4, Pp 35-56 (2022)

The Gorgan schist complex, composed of low-grade metamorphic rocks, are widespread in the Alborz highlands in the south of Mazandaran Sea and extended from Behshahr to Aliabad. The complex is characterized by alternating of phyllite, sericite, chlori

Externí odkaz: https://doaj.org/article/d8bae8c5b4d2416984f1d41b64ea486a

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Akademický článek

Geochemistry of volcanic rocks and dykes from the Remeshk-Mokhtarabad and Fannuj-Maskutan Ophiolites (Makran Accretionary Prism, SE Iran): New constraints for magma generation in the Middle East neo-Tethys

Autor: Emilio Saccani, Morteza Delavari, Asghar Dolati, Luca Pandolfi, Edoardo Barbero, Valentina Brombin, Michele Marroni

Publikováno v: Geosystems and Geoenvironment, Vol 2, Iss 3, Pp 100140- (2023)

The Remeshk-Mokhtarabad and Fannuj-Maskutan ophiolites represent two major ophiolitic units in the North Makran Domain (Makran Accretionary Prism). Volcanic rocks and dykes of these ophiolites mainly consist of basalts and rare basaltic andesites, an

Externí odkaz: https://doaj.org/article/8ca0315dd646430c845775c8826f9ba9

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Akademický článek

Geochemistry of volcanic rocks from the south of Gazik (east of Birjand): implications for the evolution of Sistan Ocean (eastern Iran)

Autor: Morteza Delavari, Asghar Dolati, Emad Alipoorian

Publikováno v: پترولوژی, Vol 8, Iss 31, Pp 21-42 (2017)

The study area is located the south of Gazik (east of Birjand) and along the eastern margin of the Sistan suture zone. The south of Gazic volcanics crop out as a north- south trending unit. They are predominantly intermediate extrusives including and

Externí odkaz: https://doaj.org/article/531f0ad80c774d83b2ff14cbfe8e24c8

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Akademický článek

The Central Alborz Permian basaltic magmatism: an evidence of southern passive continental margin of Paleo- Tethys

Autor: Morteza Delavari, Farzaneh Rostami, Asghar Dolati

Publikováno v: پترولوژی, Vol 8, Iss 29, Pp 53-74 (2017)

The study area is located in the Central Alborz (northeast of Baladeh). The Permianmagmatism in this area occurs as a basaltic unit between Ruteh-Nessen Formation.Petrographically, the rocks are plagioclase phyric and geochemically, display alkalines

Externí odkaz: https://doaj.org/article/8662325400274c81ae984e13ecd5042b

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Processes of seamount materials accretion in subduction complexes: The example of the Durkan Complex (Makran Accretionary Prism, SE Iran)

Autor: Edoardo Barbero, Maria Di Rosa, Luca Pandolfi, Morteza Delavari, Asghar Dolati, Federica Zaccarini, Emilio Saccani, Michele Marroni

Seamounts are topographic highs of the oceanic plates, and they are passively carried toward convergent margins where they may interact with the frontal part of the subduction complexes, modifying their shape and influencing the operating tectonic pr

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::caffa9ad1158461bd2835ef58beb3d47
https://doi.org/10.5194/egusphere-egu23-4276

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Nature and evolution of the Middle East Neotethys: New constraints from geochemistry and age of ophiolites and metaophiolites from the Makran Accretionary Prism (SE Iran)

Autor: Emilio Saccani, Edoardo Barbero, Luca Pandolfi, Morteza Delavari, Asghar Dolati, Michele Marroni, Rita Catanzariti, Marco Chiari

Ophiolites may originate in a variety of oceanic settings such as mid-ocean ridges, intra-oceanic and continental margin volcanic arc, marginal basins, and seamounts. Ophiolites from different settings show distinctive lithological features and geoch

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::db3ec1c6cdd30cbd7ea99ab4a7906562
https://doi.org/10.5194/egusphere-egu23-5270

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The deformation pattern of subducting seamount: insights from the structural evolution of the Late Cretaceous Durkan Complex in the North Makran domain (Makran Accretionary Prism, SE Iran)

Autor: Edoardo Barbero, Luca Pandolfi, Morteza Delavari, Asghar Dolati, Maria Di Rosa, Federica Zaccarini, Emilio Saccani, Michele Marroni

The occurrence of topographic relief along the subducting plate is thought to play a significant role in controlling the architecture and the deformation processes of subduction complexes Seamounts and seamounts chain represent topographic reliefs of

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::455bc624852e1477b794a51d19e18a9a
https://doi.org/10.5194/egusphere-egu22-3639

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The Durkan Complex in the western Makran Accretionary Prism (SE Iran): Evidence for a Late Cretaceous tectonically disrupted oceanic seamount

Autor: Rita Catanzariti, Michele Marroni, Asghar Dolati, Valeria Luciani, Edoardo Barbero, Luca Pandolfi, Emilio Saccani, Morteza Delavari, Marco Chiari

The Makran Accretionary Prism (SE of Iran) represents the less known segment of the Alpine-Himalayan orogenic system. It results from the Cretaceous to present-day convergence between the Arabian and Eurasian plates that was accommodated by the north

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7551c4a87325581ea20f244cc83c46b3
https://doi.org/10.5194/egusphere-egu2020-304

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