OCCURRENCES OF BRUCITE, SERPENTINE, FORSTERITE AND HYDROMAGNESITE BEARING MARBLES, EAST OF SHIRKUH, YAZD

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GHANEI ARDAKANI J.; MAKIZADEH M.A.

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Journal: RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE" Year:2006 | Volume:25 | Issue:3 Page(s): 39-48

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Title

OCCURRENCES OF BRUCITE, SERPENTINE, FORSTERITE AND HYDROMAGNESITE BEARING MARBLES, EAST OF SHIRKUH, YAZD

Author(s)

GHANEI ARDAKANI J. | MAKIZADEH M.A. | Issue Writer Certificate

Keywords

SHIRKUH BATHOLITEQ4

MARBLEQ3

SKARNQ3

BRUCITEQ3

HYDROMAGNESITEQ3

Abstract

Due to post Cretaceus intrusions, various MARBLE-skarn mineralizations are formed in eastern Shirkuh Fault Zone. MARBLEs constitute the last zone in cantact metamorphic aureole. MARBLEs are characterized by following mineral assemblages: BRUCITE+serpentine+forstrite+hydromagnesite+calcite+dolomite.The MARBLEs are undergone to pyroxene hornfels facies with the temperature between 450˚c to 600˚c (p<2kb).The study has shown the paragenesis and texture relation of minerals as well as the three stages of decarbonation, hydration and carbonation.

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APA: Copy

GHANEI ARDAKANI, J., & MAKIZADEH, M.A.. (2006). OCCURRENCES OF BRUCITE, SERPENTINE, FORSTERITE AND HYDROMAGNESITE BEARING MARBLES, EAST OF SHIRKUH, YAZD. RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE", 25(3), 39-48. SID. https://sid.ir/paper/55886/en

Vancouver: Copy

GHANEI ARDAKANI J., MAKIZADEH M.A.. OCCURRENCES OF BRUCITE, SERPENTINE, FORSTERITE AND HYDROMAGNESITE BEARING MARBLES, EAST OF SHIRKUH, YAZD. RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE"[Internet]. 2006;25(3):39-48. Available from: https://sid.ir/paper/55886/en

IEEE: Copy

J. GHANEI ARDAKANI, and M.A. MAKIZADEH, “OCCURRENCES OF BRUCITE, SERPENTINE, FORSTERITE AND HYDROMAGNESITE BEARING MARBLES, EAST OF SHIRKUH, YAZD,” RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE", vol. 25, no. 3, pp. 39–48, 2006, [Online]. Available: https://sid.ir/paper/55886/en

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