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Title

Petrology, geochemistry and tectonomagmatic setting of Zajkan granitoid (Tarom-Hashtjin sub-zone, West of Qazvin)

Pages

  79-100

Abstract

Zajkan area as a part of Tarom-Hashtjin magmatic belt is dominated by some granitic intrusions intruding the Eocene volcano-sedimentary rocks. The Eocene volcano-sedimentary rocks are as alternation of acidic to intermediate tuffs and lavas. These intrusions composed of gabbro, pyroxene quartz monzodiorite, pyroxene quartz monzonite and granodiorite with high-K calc-alkaline composition and I-type metaluminous nature. On the spider diagrams, the studied rocks have similar trace elements patterns indication of their genetic relation. The rocks also display LILEs enriched along with negative HFSEs anomalies. Based on chondrite-normalized REE patterns, these intrusions are characterized by LREE enrichment, high LREE/HREE and LaN/YbN (6. 1-9. 1). The overall field investigation, petrological and geochemical studies, as well as tectonic setting discrimination diagrams show that the Zajkan intrusions were possibly formed from a subduction related metasomatized lithospheric mantle in a post-collisional setting.

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    APA: Copy

    Seyedqaraeini, Abbas, MOKHTARI, MIR ALI ASGHAR, & KOUHESTANI, HOSSEIN. (2019). Petrology, geochemistry and tectonomagmatic setting of Zajkan granitoid (Tarom-Hashtjin sub-zone, West of Qazvin). PETROLOGY, 10(39 ), 79-100. SID. https://sid.ir/paper/404243/en

    Vancouver: Copy

    Seyedqaraeini Abbas, MOKHTARI MIR ALI ASGHAR, KOUHESTANI HOSSEIN. Petrology, geochemistry and tectonomagmatic setting of Zajkan granitoid (Tarom-Hashtjin sub-zone, West of Qazvin). PETROLOGY[Internet]. 2019;10(39 ):79-100. Available from: https://sid.ir/paper/404243/en

    IEEE: Copy

    Abbas Seyedqaraeini, MIR ALI ASGHAR MOKHTARI, and HOSSEIN KOUHESTANI, “Petrology, geochemistry and tectonomagmatic setting of Zajkan granitoid (Tarom-Hashtjin sub-zone, West of Qazvin),” PETROLOGY, vol. 10, no. 39 , pp. 79–100, 2019, [Online]. Available: https://sid.ir/paper/404243/en

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