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Information Journal Paper

Title

Physicochemical Attributes of Parental Magma in Collisional Porphyry Copper Systems; Using Biotite Chemistry, Case Study: Chahfiruzeh Porphyry Copper Deposit

Pages

  561-586

Abstract

 Almost all of the well-known porphyry copper deposits in Iran occur within the Kerman Cenozoic Magmatic Arc (KCMA) (Fig 1) in the southeastern part of Cenozoic Urumieh– Dokhtar magmatic belt (Hassanpour et al., 2015). The Miocene Chahfiruzeh porphyry copper deposit as an example of collisional porphyry intrusion is located in the Kerman Cenozoic Magmatic Arc (Fig 2) (Einali et al., 2014). In this research, we attempt to characterize the Physicochemical Attributes of parental magma in the Chahfiruzeh porphyry deposit, using chemistry of magmatic Biotite. . . .

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    APA: Copy

    HEIDARI, MAJID, ZARASVANDI, ALIREZA, REZAEI, MOHSEN, Raith, Johann, & SAKI, ADEL. (2019). Physicochemical Attributes of Parental Magma in Collisional Porphyry Copper Systems; Using Biotite Chemistry, Case Study: Chahfiruzeh Porphyry Copper Deposit. JOURNAL OF ECONOMIC GEOLOGY, 10(2 ), 561-586. SID. https://sid.ir/paper/180489/en

    Vancouver: Copy

    HEIDARI MAJID, ZARASVANDI ALIREZA, REZAEI MOHSEN, Raith Johann, SAKI ADEL. Physicochemical Attributes of Parental Magma in Collisional Porphyry Copper Systems; Using Biotite Chemistry, Case Study: Chahfiruzeh Porphyry Copper Deposit. JOURNAL OF ECONOMIC GEOLOGY[Internet]. 2019;10(2 ):561-586. Available from: https://sid.ir/paper/180489/en

    IEEE: Copy

    MAJID HEIDARI, ALIREZA ZARASVANDI, MOHSEN REZAEI, Johann Raith, and ADEL SAKI, “Physicochemical Attributes of Parental Magma in Collisional Porphyry Copper Systems; Using Biotite Chemistry, Case Study: Chahfiruzeh Porphyry Copper Deposit,” JOURNAL OF ECONOMIC GEOLOGY, vol. 10, no. 2 , pp. 561–586, 2019, [Online]. Available: https://sid.ir/paper/180489/en

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