MINERAL CHEMISTRY OF GARNET IN PEGMATITE AND METAMORPHIC ROCKS IN THE HAMEDAN AREA

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AHMADI KHALAJI AHMAD; TAHMASBI ZAHRA

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Journal: JOURNAL OF ECONOMIC GEOLOGY Year:2016 | Volume:7 | Issue:2 Page(s): 243-258

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Title

MINERAL CHEMISTRY OF GARNET IN PEGMATITE AND METAMORPHIC ROCKS IN THE HAMEDAN AREA

Author(s)

AHMADI KHALAJI AHMAD | TAHMASBI ZAHRA | Issue Writer Certificate

Keywords

HAMEDANQ2

METAMORPHICQ2

GARNETQ2

ZONINGQ2

Abstract

IntroductionThe area of this study is located near Hamadan within the Sanandaj - Sirjan tectonic zone. In the Hamadan area, consisting mainly of Mesozoic plutonic and METAMORPHIC rocks, aplites and pegmatites locally contain GARNETs. (Baharifar et al., 2004, Amidi and Majidi, 1977; Torkian, 1995. GARNET-bearing schists and hornfelses in the area are products of regional metamorphism shown by slate and phyllite (Baharifar, 2004). In this investigation the distribution of elements in GARNET in different rock type was studied to determine their mineral types and conditions of formation. GARNET samples from igneous and METAMORPHIC rocks were analyzed by electron microprobe (EMPA), the results of which are presented in this article.

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APA: Copy

AHMADI KHALAJI, AHMAD, & TAHMASBI, ZAHRA. (2016). MINERAL CHEMISTRY OF GARNET IN PEGMATITE AND METAMORPHIC ROCKS IN THE HAMEDAN AREA. JOURNAL OF ECONOMIC GEOLOGY, 7(2), 243-258. SID. https://sid.ir/paper/180544/en

Vancouver: Copy

AHMADI KHALAJI AHMAD, TAHMASBI ZAHRA. MINERAL CHEMISTRY OF GARNET IN PEGMATITE AND METAMORPHIC ROCKS IN THE HAMEDAN AREA. JOURNAL OF ECONOMIC GEOLOGY[Internet]. 2016;7(2):243-258. Available from: https://sid.ir/paper/180544/en

IEEE: Copy

AHMAD AHMADI KHALAJI, and ZAHRA TAHMASBI, “MINERAL CHEMISTRY OF GARNET IN PEGMATITE AND METAMORPHIC ROCKS IN THE HAMEDAN AREA,” JOURNAL OF ECONOMIC GEOLOGY, vol. 7, no. 2, pp. 243–258, 2016, [Online]. Available: https://sid.ir/paper/180544/en

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