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Information Journal Paper

Title

GEOCHEMISTRY AND SOURCE DETERMINATION OF TOURMALINES IN BOROUJERD AREA

Pages

  281-292

Abstract

 The study of MICROPROBE ANALYSES in different TOURMALINE bearing unites in BOROUJERD area, for example, quartz TOURMALINE veins in Nezamabad quartz diorites, Aplitepegmatite TOURMALINE bearing Ghalesamorkhan, Gijali and Kabotarlan granodiorites, pegmatite veins in Kolahjob schist and nodular TOURMALINE in Dehgah and ASTANEH show that most TOURMALINEs in BOROUJERD area are schorlite. Needle like Ghalae Samorkhan and some samples from Kolahjob-Gijali are foitite. Euhedral and none zoning, high Fe/Fe+Mg, low X site vacancy and high Al amount in more of TOURMALINE are reasons of magmatic source. The occurrence of TOURMALINE in peraluminous granite Dehgah and ASTANEH is evidence of enriched B magma source. Therefor, the studied area TOURMALINEs depend of granitic source and originate of hydrothermal fluid to magmatic source.

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    Cite

    APA: Copy

    MIRSEPAHVANAD, F., TAHMASBI, Z., SHAHROKHI, S.V., AHMADI KHALAJI, A., & KHALILI, M.. (2012). GEOCHEMISTRY AND SOURCE DETERMINATION OF TOURMALINES IN BOROUJERD AREA. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 20(2), 281-292. SID. https://sid.ir/paper/4120/en

    Vancouver: Copy

    MIRSEPAHVANAD F., TAHMASBI Z., SHAHROKHI S.V., AHMADI KHALAJI A., KHALILI M.. GEOCHEMISTRY AND SOURCE DETERMINATION OF TOURMALINES IN BOROUJERD AREA. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2012;20(2):281-292. Available from: https://sid.ir/paper/4120/en

    IEEE: Copy

    F. MIRSEPAHVANAD, Z. TAHMASBI, S.V. SHAHROKHI, A. AHMADI KHALAJI, and M. KHALILI, “GEOCHEMISTRY AND SOURCE DETERMINATION OF TOURMALINES IN BOROUJERD AREA,” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 20, no. 2, pp. 281–292, 2012, [Online]. Available: https://sid.ir/paper/4120/en

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