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C R Geosci Several episodes of magmatic activity have been identified in Iran. The belt is composed of about 10 kilometres of Mesozoic and Tertiary sediments mostly carbonates and, like the Zagros, was folded into long linear northwest-southeast trending folds during the last phase of the Alpine Orogeny, in the Miocene and Plio-Pleistocene time. Deposition of shallow marine sediments covered large areas in Iran during Paleozoic e. Volcanic and plutonic rocks with an age of — million years have been reported from many localities in Iran, particularly in Central Iran and Azerbaijan. This orogenic episode generated the Tabriz fault, extending in a northwest—southeast direction from Zanjan depression to the northern mountains of Tabriz Mishu, Morou and northwest of Azerbaijan and the Caucasus. Views Read Edit View history.

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This page was last edited on 18 April , at Alavi M Sedimentary and structural characteristics of the paleo-Tethys remnants in northeastern Iran. The northern part is characterized by dominance of east—west trending faults, Bashagard fault being the most important one. It was deformed and largely consolidated by the Early Cimmerian folding and the Late Alpine folding. The legacy of Mike Coward. The Quaternary volcanism produced very high peaks such as Sahand , Sabalan , Damavand , Taftan , Bazman and many others. GSA Abstr Prog

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Stampfli GM, Borel GD A plate tectonic model for the Paleozoic and Mesozoic constrained by dynamic plate boundaries and restored synthetic oceanic isochrons. The northeastern active fold belt of Iran, the Kopet Dagh , is formed on the Hercynian metamorphosed basement at the southwestern margin of the Turan Platform. This is a preview of subscription content, log in to check access. Hf isotope evidence from juvenile rocks through time. Iranian microplates east and northeast of the Zagros were detached from Gondwana in the Carboniferous during this orogenic phase. The Hf model ages of the Hasan-Robat zircons is within the range of those reported from the Cadomian granitoids in Iran. In the east, it is separated from Flysch Zone by the Nehbandan fault, whereas the western boundary with Central Iran is Nayband fault and Shotori Mountains. The basement is likely composed of an oceanic crust.

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Its western boundary is Minab fault; to the south, it is restricted by the Gulf of Oman , and to the east, it extends into Pakistan. These rocks are widespread in Takab and Anarak Regions. In Kalmard area, Ordovician sediments are sitting on the Vendian sediments through an angular unconformity.

If you are looking for Iranian men and wish to contact somebody online then join Loveawake free dating casual or long-term Meet marriage-minded men. Petrology and geochemistry of the granitoid complex of Boroujerd, Sanandaj-Sirjan Zone, They represent new precise U–Pb single zircon dating Long term.

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