MINERALOGY OF BRUCITE BEARING MARBLES, EASTERN MARGIN OF SHIRKUH BATHOLITH (WEST OF YAZD PROVINCE)

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Journal: Iranian Journal of Crystallography and Mineralogy Year:2002 | Volume:9 | Issue:2 Page(s): 117-125

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Information Journal Paper

Title

MINERALOGY OF BRUCITE BEARING MARBLES, EASTERN MARGIN OF SHIRKUH BATHOLITH (WEST OF YAZD PROVINCE)

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Keywords

SKARN-MARBLEQ2

BRUCITEQ4

HYDROMAGNESITEQ3

Abstract

Igneous bodies in Manshad-Taft fault zone are intruded into Shirkuh granitic batholitic basement. They also cause different SKARN-MARBLE mineralization in dolomitized limestones which are covered granitic basement. Skarns are composed of variety of minerals. Marbles consist of various minerals such as BRUCITE, forsterite, diopsid, periclase, talc, calcite, dolomite, and HYDROMAGNESITE. Petrographic and geochemical data have revealed that there is several stages during the formation of marble minerals. At the first stage, anhydrous minerals formed, then followed byhydrous assemblage. Generation of BRUCITE occurs at the second stage and is due to late hydrothermal system withlow XCO2 and high XH2O fluids. HYDROMAGNESITE deposition is occured by oxidation of BRUCITE.

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معرفی کانی شناسی اسکارن کوه در با تاکید برکانی کمیابت کلینتوتیت، کوهستان شیر کوه - یزد

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APA: Copy

. (2002). MINERALOGY OF BRUCITE BEARING MARBLES, EASTERN MARGIN OF SHIRKUH BATHOLITH (WEST OF YAZD PROVINCE). IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 9(2), 117-125. SID. https://sid.ir/paper/4067/en

Vancouver: Copy

. MINERALOGY OF BRUCITE BEARING MARBLES, EASTERN MARGIN OF SHIRKUH BATHOLITH (WEST OF YAZD PROVINCE). IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2002;9(2):117-125. Available from: https://sid.ir/paper/4067/en

IEEE: Copy

, “MINERALOGY OF BRUCITE BEARING MARBLES, EASTERN MARGIN OF SHIRKUH BATHOLITH (WEST OF YAZD PROVINCE),” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 9, no. 2, pp. 117–125, 2002, [Online]. Available: https://sid.ir/paper/4067/en

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