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Information Journal Paper

Title

PETROGRAPHY AND PETROLOGY OF A-TYPE GRANITOIDS OF EASTERN MISHO MOUNTAINS WITH EMPHASIS ON THEIR GEODYNAMIC IMPORTANCE

Pages

  529-544

Abstract

 Granitoidic bodies of the eastern MISHO MOUNTAINS (SW Marand-East Azerbaidjan) have intruded into Kahar Formation and mafic-ultramafic rocks of MISHO MOUNTAINS and has faulty contact with Triassic carbonate deposits. The composition of these bodies ranges from quartz monzonite to granite and alkali-granite and it is cut by porphyritic granitic and diabasic dykes. The main minerals of these bodies are pertitic alkali feldspar, quartz and Na-rich plagioclase, accompanied by lesser amounts of biotite and amphibole. In this regard, these bodies belong to HYPERSOLVUS granitoids and A2 sub-group of A-TYPE GRANITOIDs. The parental magma of these bodies has calc-alkaline to shoshonitic characteristic and show positive anomalies of LILE and LREE, and obvious negative anomalies of Ba, Eu, and HREE. These bodies have emplaced in a POST-COLLISIONAL tectonic setting related to tensional movements after HERCYNIAN orogenic phase and have formed by melting of crustal rocks.

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    APA: Copy

    MOAYYED, M., & HOSSEINZADEH, GH.. (2011). PETROGRAPHY AND PETROLOGY OF A-TYPE GRANITOIDS OF EASTERN MISHO MOUNTAINS WITH EMPHASIS ON THEIR GEODYNAMIC IMPORTANCE. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 19(3), 529-544. SID. https://sid.ir/paper/3999/en

    Vancouver: Copy

    MOAYYED M., HOSSEINZADEH GH.. PETROGRAPHY AND PETROLOGY OF A-TYPE GRANITOIDS OF EASTERN MISHO MOUNTAINS WITH EMPHASIS ON THEIR GEODYNAMIC IMPORTANCE. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2011;19(3):529-544. Available from: https://sid.ir/paper/3999/en

    IEEE: Copy

    M. MOAYYED, and GH. HOSSEINZADEH, “PETROGRAPHY AND PETROLOGY OF A-TYPE GRANITOIDS OF EASTERN MISHO MOUNTAINS WITH EMPHASIS ON THEIR GEODYNAMIC IMPORTANCE,” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 19, no. 3, pp. 529–544, 2011, [Online]. Available: https://sid.ir/paper/3999/en

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