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Information Journal Paper

Title

Relation of alkali-metasomatism and Ti-REE-U (Th) mineralization in the Saghand mining district, Central Iran

Pages

  471-496

Abstract

 The Saghand mining district is a part of Bafq-Saghand metallogenic zone in the Central Iranian geostructural zone which is located in northeast of city of Yazd. This area is known to be more susceptible to mineralization of U and Th radioactive elements, but in fact is that its main importance is for relatively large iron deposits. . .

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  • Cite

    APA: Copy

    DEYMAR, SALEH, BEHZADI, MEHRDAD, YAZDI, MOHAMMAD, & Rezvanianzadeh, Mohammad Reza. (2019). Relation of alkali-metasomatism and Ti-REE-U (Th) mineralization in the Saghand mining district, Central Iran. JOURNAL OF ECONOMIC GEOLOGY, 10(2 ), 471-496. SID. https://sid.ir/paper/180490/en

    Vancouver: Copy

    DEYMAR SALEH, BEHZADI MEHRDAD, YAZDI MOHAMMAD, Rezvanianzadeh Mohammad Reza. Relation of alkali-metasomatism and Ti-REE-U (Th) mineralization in the Saghand mining district, Central Iran. JOURNAL OF ECONOMIC GEOLOGY[Internet]. 2019;10(2 ):471-496. Available from: https://sid.ir/paper/180490/en

    IEEE: Copy

    SALEH DEYMAR, MEHRDAD BEHZADI, MOHAMMAD YAZDI, and Mohammad Reza Rezvanianzadeh, “Relation of alkali-metasomatism and Ti-REE-U (Th) mineralization in the Saghand mining district, Central Iran,” JOURNAL OF ECONOMIC GEOLOGY, vol. 10, no. 2 , pp. 471–496, 2019, [Online]. Available: https://sid.ir/paper/180490/en

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