Geochemistry and zircon U-Pb geochronology of Miocene plutons in the Urumieh-Dokhtar magmatic arc,east Tafresh,Central Iran |
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Authors: | Davood Raeisi Hassan Mirnejad Christopher McFarlane Maryam Sheibi Shahrouz Babazadeh |
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Institution: | 1. Department of Geology, Faculty of Science, University of Tehran , Tehran, Iran d.raeisi@ut.ac.ir;3. Department of Geology, Faculty of Science, University of Tehran , Tehran, Iran;4. Department of Geology and Environmental Earth Sciences, Miami University , Oxford, OH, USA;5. Department of Geology, University of New Brunswick , Fredericton, New Brunswick, Canada;6. Faculty of Earth Sciences, Shahrood University of Technology , Shahrood, Iran;7. Research Institute for Earth Sciences, Geological Survey of Iran , Tehran, Iran |
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Abstract: | ABSTRACT The Tafresh plutons that include Ahmadabab diorite, Vasfonjerd monzonite, Mehrezamin diorite and Chahak diorite, located to the east of Tafresh city, north-central Iran, are part of Urumieh-Dokhtar magmatic arc. U-Pb dating of zircon grains provides emplacement ages of 22.3 ± 1 Ma for the Ahmadabad diorite, and tightly clustered ages of 22.2 ± 0.2 Ma, 21.3 ± 0.2 Ma, and 21.7 ± 0.4 Ma for Vasfonjerd monzodiorite, Mehrezamin diorite-monzonite, and Chahak diorite-monzonite plutons, respectively. These rocks are metaluminous to weakly peraluminous, calc-alkaline, and characterized by enrichment in light rare earth elements, Nb-Ta negative anomalies, and high LILE/HFSE ratios. Tafresh plutonic rocks originated from a parental magma source and experienced different degrees of partial melting. Geochemical signatures of Tafresh plutonic rocks, such as a wide range of Y/Nb (2.7–8.4) and low Zr/Nb (19.5–35.) ratios, Nb/Ta (11.46–18.15), argue for mantle–crust interaction during generation of Tafresh magmas. Relatively low Nb/La ratios further indicate that the lithospheric mantle played a significant role in melt generation. HREE signatures (i.e. decrease Dy/Yb with increasing SiO2) preclude substantial involvement of garnet either in the residue, both during partial melting and fractionation of the magma. The plutons are a product of final stages of subduction-related magmatism prior to the collision between the Arabian and Eurasian tectonic plates. |
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Keywords: | UrumiehDokhtar magmatic arc emplacement ages calcalkaline mantle crust interaction subduction |
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