Zobrazeno 1 - 10
of 19
pro vyhledávání: '"Sasan Bagheri"'
Publikováno v:
Iranian Journal of Crystallography and Mineralogy. 29:149-164
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::72be0eb426e3aee7edf839a906d9d6bd
https://doi.org/10.52547/ijcm.29.1.149
https://doi.org/10.52547/ijcm.29.1.149
Autor:
Elham Bahramnejad, Sasan Bagheri, Mortaza Sharifi, Nusret Nurlu, Yuruo Shi, Ghodrat Torabi, Moussa Noghreyan
Publikováno v:
Geochemistry. :125988
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0627624181af8e1831d312473d33a21e
https://doi.org/10.1016/j.chemer.2023.125988
https://doi.org/10.1016/j.chemer.2023.125988
Autor:
Mostafa Ghomashi, Mohammad Hossein Adabi, Seyedeh Narges Edalatimanesh, Sasan Bagheri, Mohammad Boomeri
Publikováno v:
Researches in Earth Sciences. 11:47-71
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5c01f98f7615a60e0b2f4a67decec8d7
https://doi.org/10.52547/esrj.11.1.47
https://doi.org/10.52547/esrj.11.1.47
Publikováno v:
Lithos. :106864
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::38a7aa68f7bd7dfecd77590e992e29f8
https://doi.org/10.1016/j.lithos.2022.106864
https://doi.org/10.1016/j.lithos.2022.106864
Publikováno v:
Iranian Journal of Crystallography and Mineralogy. 27:281-294
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c76b9fbb7c41c915219fbd02ab6b446a
https://doi.org/10.29252/ijcm.27.2.281
https://doi.org/10.29252/ijcm.27.2.281
Publikováno v:
Ore Geology Reviews. 104:477-494
The Lar porphyry Cu-Mo deposit is located 20 km northeast of Zahedan in the Sistan Suture Zone (SSZ), in the southeastern part of Iran. Lar is a sub-economic porphyry Cu-Mo deposit with average grades of 0.16% Cu, 0.01% Mo, and 0.66 ppb Au. The Cu-Mo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::78d05ab47e424efeef215a3b5277e9f7
https://doi.org/10.1016/j.oregeorev.2018.11.018
https://doi.org/10.1016/j.oregeorev.2018.11.018
Autor:
Abdul Qayyum, Nalan Lom, Hossein Azizi, Douwe J.J. van Hinsbergen, Emad Rojhani, Farzin Ghaemi, Sasan Bagheri
The Eastern Iranian Orocline provides us several opportunities to study magmatism in relation to tectonic events. The buckling of this orocline is accompanied by an extreme extension in its Khorasan outer arc during which a calc-alkaline dike swarm,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0cef3bbf6de96ddb62b45c9aab3baf93
https://doi.org/10.5194/egusphere-egu21-14258
https://doi.org/10.5194/egusphere-egu21-14258
Publikováno v:
Geologos, Vol 26, Iss 1, Pp 51-64 (2020)
The Oligocene Lar igneous complex is located in the Sistan suture zone of Iran, being emplaced in Paleocene to Eocene flysch-type rocks. This complex includes mainly intermediate K-rich volcanic (trachyte, latite and andesite) and plutonic (syenite a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::624141b611271a2a8905b165f86d6710
https://hdl.handle.net/10593/25806
https://hdl.handle.net/10593/25806
Publikováno v:
Resource Geology. 66:286-302
The Mesozoic Bazman granitoids are located in Sistan and Baluchestan province, southeastern Iran. Geology of the study area consists of Carboniferous shale, sandstone, and limestone and Permian siltstone, shale, sandstone, limestone, and dolomite tha
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cfd3f63af2ba345561657074753f30ea
https://doi.org/10.1111/rge.12102
https://doi.org/10.1111/rge.12102
Autor:
Sasan Bagheri, Shamsoddin Damani Gol
Publikováno v:
Earth-Science Reviews. 210:103322
The Eastern Iranian range is seen as a large scale India-Eurasia collisional event and the subsequent amalgamation of the Afghan and Lut micro-continents, including the Neo-Tethyan accretionary complexes and associated island arcs. Revised examinatio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4594c470b5376748ed896f98c8bbce67
https://doi.org/10.1016/j.earscirev.2020.103322
https://doi.org/10.1016/j.earscirev.2020.103322