Research Article| March 01, 1980 Tectonostratigraphic evolution of the Zagrosides of Iran Mehdi Alavi Mehdi Alavi 1Geology Department, College of Arts and Sciences, Shiraz University, Shiraz, Iran Search for other works by this author on: GSW Google Scholar Author and Article Information Mehdi Alavi 1Geology Department, College of Arts and Sciences, Shiraz University, Shiraz, Iran Publisher: Geological Society of America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1980) 8 (3): 144–149. https://doi.org/10.1130/0091-7613(1980)8<144:TEOTZO>2.0.CO;2 Article history First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Mehdi Alavi; Tectonostratigraphic evolution of the Zagrosides of Iran. Geology 1980;; 8 (3): 144–149. doi: https://doi.org/10.1130/0091-7613(1980)8<144:TEOTZO>2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract A new tectonostratigraphic model is proposed for the evolution of the Zagrosides of Iran. The Zagros thrust line is considered to be a reactivated high-angle reverse fault. The suture between the Iranian and Arabian continents is inferred to be along the southwestern front of the Urmia-Dokhtar magmatic arc. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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Mehdi Alavi (1980) studied this question.