COMPARISON BETWEEN THE CHEMISTRY OF IGNEOUS AND HYDROTHERMAL BIOTITE IN THE IGNEOUS ROCKS OF SAKHTEHESAR MOUNTAIN

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AYATI F.; MAHDEVARI S.

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Journal: JOURNAL OF ECONOMIC GEOLOGY Year:2010 | Volume:1 | Issue:1 Page(s): 117-134

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Title

COMPARISON BETWEEN THE CHEMISTRY OF IGNEOUS AND HYDROTHERMAL BIOTITE IN THE IGNEOUS ROCKS OF SAKHTEHESAR MOUNTAIN

Author(s)

AYATI F. | MAHDEVARI S. | Issue Writer Certificate

Keywords

BIOTITEQ2

HYDROTHERMALQ2

SAKHTEHESARQ3

Abstract

Sakhtehesar Mountain is located in Urumieh-Dokhtar magmatic belt and is composed of volcanic and subvolcanic rocks (Pliocene andesite to dacite) which intruded the volcanics and pyroclastics of Paleocene age. Three alteration zones including potassic, phyllic and propylitic are recognized in the area. In this paper, the mineral chemistry of magmatic and primary BIOTITE and the mineral chemistry of BIOTITE in potassic and phyllic alteration zones have been studied. Investigations show that primary and secondary BIOTITEs are different from each other and HYDROTHERMAL fluids associated with the potassic alteration are distinctively different from the fluids associated with the phyllic alteration zone in the area.

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References

PRELIMINARY REPORT OF PORPHYRY CU EXPLORATION AT CENTRAL PROVINCE OF IRAN

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APA: Copy

AYATI, F., & MAHDEVARI, S.. (2010). COMPARISON BETWEEN THE CHEMISTRY OF IGNEOUS AND HYDROTHERMAL BIOTITE IN THE IGNEOUS ROCKS OF SAKHTEHESAR MOUNTAIN. JOURNAL OF ECONOMIC GEOLOGY, 1(1), 117-134. SID. https://sid.ir/paper/180553/en

Vancouver: Copy

AYATI F., MAHDEVARI S.. COMPARISON BETWEEN THE CHEMISTRY OF IGNEOUS AND HYDROTHERMAL BIOTITE IN THE IGNEOUS ROCKS OF SAKHTEHESAR MOUNTAIN. JOURNAL OF ECONOMIC GEOLOGY[Internet]. 2010;1(1):117-134. Available from: https://sid.ir/paper/180553/en

IEEE: Copy

F. AYATI, and S. MAHDEVARI, “COMPARISON BETWEEN THE CHEMISTRY OF IGNEOUS AND HYDROTHERMAL BIOTITE IN THE IGNEOUS ROCKS OF SAKHTEHESAR MOUNTAIN,” JOURNAL OF ECONOMIC GEOLOGY, vol. 1, no. 1, pp. 117–134, 2010, [Online]. Available: https://sid.ir/paper/180553/en

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