ELEMENTS VARIATIONS AND THE ORIGIN OF FLUIDS DURING THE HYDROTHERMAL ALTERATIONS IN THE ASTANEH-ARAK GRANITOID

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MIKAILI RAHIMEH; KALIMI NOGHREYAN MOUSSA; MACKIZADEH MOHAMMAD ALI; TAGHIPOUR BATOUL

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Journal: PETROLOGY Year:2011 | Volume:2 | Issue:7 Page(s): 119-134

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Title

ELEMENTS VARIATIONS AND THE ORIGIN OF FLUIDS DURING THE HYDROTHERMAL ALTERATIONS IN THE ASTANEH-ARAK GRANITOID

Author(s)

MIKAILI RAHIMEH | KALIMI NOGHREYAN MOUSSA | MACKIZADEH MOHAMMAD ALI | TAGHIPOUR BATOUL | Issue Writer Certificate

Keywords

GRANITOIDQ3

ASTANEHQ2

HYDROTHERMALQ3

STABLE ISOTOPEQ2

ELEMENT MOBILITYQ2

Abstract

Seven distinct HYDROTHERMAL alteration zones developed within the ASTANEH GRANITOID.The phyllic and silicic alterations have a wide extension in the study area. In the phyllic alteration, La in comparison to other REE's, is much more enriched which may be the result of sericite formation. The enrichment of LREE in the propylitic alteration, due to their accommodation in secondary minerals, is more than that of unaltered sample. The REE normalized pattern in the argillic alteration shows a considerable leaching of REE during the alteration process. The Eu/Eu* ratio in the altered samples is less than one and in comparison to unaltered sample displays positive anomaly. Generally, the chondrite normalized pattern in altered and unaltered sample is similar. The STABLE ISOTOPEs, dO18 and dD, data indicate that magmatic-metamorphic waters were responsible for fluids involved in phyllic and silicic alterations.

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References

MINERALS CHEMISTRY AND GEOCHEMISTRY OF PROPYLITIC ALTERATION IN ASTANEH GRANITOID (SOUTHWEST ARAK)

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APA: Copy

MIKAILI, RAHIMEH, KALIMI NOGHREYAN, MOUSSA, MACKIZADEH, MOHAMMAD ALI, & TAGHIPOUR, BATOUL. (2011). ELEMENTS VARIATIONS AND THE ORIGIN OF FLUIDS DURING THE HYDROTHERMAL ALTERATIONS IN THE ASTANEH-ARAK GRANITOID. PETROLOGY, 2(7), 119-134. SID. https://sid.ir/paper/196997/en

Vancouver: Copy

MIKAILI RAHIMEH, KALIMI NOGHREYAN MOUSSA, MACKIZADEH MOHAMMAD ALI, TAGHIPOUR BATOUL. ELEMENTS VARIATIONS AND THE ORIGIN OF FLUIDS DURING THE HYDROTHERMAL ALTERATIONS IN THE ASTANEH-ARAK GRANITOID. PETROLOGY[Internet]. 2011;2(7):119-134. Available from: https://sid.ir/paper/196997/en

IEEE: Copy

RAHIMEH MIKAILI, MOUSSA KALIMI NOGHREYAN, MOHAMMAD ALI MACKIZADEH, and BATOUL TAGHIPOUR, “ELEMENTS VARIATIONS AND THE ORIGIN OF FLUIDS DURING THE HYDROTHERMAL ALTERATIONS IN THE ASTANEH-ARAK GRANITOID,” PETROLOGY, vol. 2, no. 7, pp. 119–134, 2011, [Online]. Available: https://sid.ir/paper/196997/en

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