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Dehghani Dashtabi S, rahgoshay M, Mohammadi S. Geochemistry of biotite and its formation conditions in Hararan granitoid. www.ijcm.ir 2023; 31 (4) :697-708
URL: http://ijcm.ir/article-1-1847-en.html
URL: http://ijcm.ir/article-1-1847-en.html
1- Department of Petrology, Faculty of Earth Sciences, Shahid Beheshti university
2- Department of Geochemistry, Faculty of Earth Science, Kharazmi University, Tehran, Iran
2- Department of Geochemistry, Faculty of Earth Science, Kharazmi University, Tehran, Iran
Abstract: (1257 Views)
Biotite is usually formed as a rock-forming mineral in a wide range of felsic to intermediate intrusive rocks. Due to complex crystal structure of biotite, different elements can substitute in this rock-forming mineral; therefore can record the physicochemical conditions of the source magma. Based on the chemical classification of mica, the biotites of the igneous rocks, investigated in the Hararan area, can be placed between the poles of phlogopite and annite, and are magnesium type, which indicates their formation in high oxygen fugacity, and according to the amounts of Mg, TiO2 and FeO oxides, these biotites are primary type. These biotites belong to the calc-alkaline magmatic series formed in the subduction environment. Based on the chemistry of biotites, oxygen fugacity in the source magma of Hararan granitoid is in the range of iron oxide. Geothermometry of biotites shows that these biotites formed at temperature ranging between 680 to 780 degrees Celsius and pressure of 2 (1-2) Kbars.
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