FACIES, STABLE ISOTOPS, AND GENESIS OF KUH-E-SURMEHPB-ZN DEPOSIT (DALAN FORMATION) IN THE SOUTH OF FIROUZABAD, FARS PROVINCE

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POUSTI M.; RASA H.; ADAABI M.H.

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Journal: GEOSCIENCES Year:2005 | Volume:15 | Issue:57 Page(s): 40-53

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Information Journal Paper

Title

FACIES, STABLE ISOTOPS, AND GENESIS OF KUH-E-SURMEHPB-ZN DEPOSIT (DALAN FORMATION) IN THE SOUTH OF FIROUZABAD, FARS PROVINCE

Author(s)

POUSTI M. | RASA H. | ADAABI M.H. | Issue Writer Certificate

Keywords

FACIESQ2

STABLE ISOTOPESQ2

PB-ZNQ2

KUH -E-SURMEHQ4

Abstract

Pb-Zn ore deposit in Kuh-e-Surmeh is located at about 33 km, south of Firouzabad. The host rocks of the ore are dolostones of the lower; part of Dalan Formation. The ore body in the dolostones occurs in three ore-bearing horizons. The main FACIES in the area are as follows: siltstone, sandstone, biomicrite, intrasparite, dolomicrosparite, dolosparite, dolomicrite, gypsum and anhydrite. Dolosparite is the main FACIES in the main ore horizons. Siliciclastic and carbonate FACIES are deposited in intertidal to supratidal environment. The mineralogy of the deposit consists of sphalerite, galena, pyrite, cerrusite, anglesite, covellite, azurite, hematite, chalcocite, dolomite, calcite, barite, and gypsum. Mineralization occures as void filling, replacement and dissemination fabrics. In some cases ore deposits fills dissolution breccia and fractures. Stable isotope studies show that dolomite has been altered by fluids with relatively high salinity and temperature of about 100C° . Field observation, texture and structure of ore bodies, type of carbonate FACIES, paragenetic sequences, fluid inclusions and oxygen and carbon isotopes indicate that Kuh-e-Surmeh PB-ZN deposits is similar to MVT type deposits.

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APA: Copy

POUSTI, M., RASA, H., & ADAABI, M.H.. (2005). FACIES, STABLE ISOTOPS, AND GENESIS OF KUH-E-SURMEHPB-ZN DEPOSIT (DALAN FORMATION) IN THE SOUTH OF FIROUZABAD, FARS PROVINCE. GEOSCIENCES, 15(57), 40-53. SID. https://sid.ir/paper/31645/en

Vancouver: Copy

POUSTI M., RASA H., ADAABI M.H.. FACIES, STABLE ISOTOPS, AND GENESIS OF KUH-E-SURMEHPB-ZN DEPOSIT (DALAN FORMATION) IN THE SOUTH OF FIROUZABAD, FARS PROVINCE. GEOSCIENCES[Internet]. 2005;15(57):40-53. Available from: https://sid.ir/paper/31645/en

IEEE: Copy

M. POUSTI, H. RASA, and M.H. ADAABI, “FACIES, STABLE ISOTOPS, AND GENESIS OF KUH-E-SURMEHPB-ZN DEPOSIT (DALAN FORMATION) IN THE SOUTH OF FIROUZABAD, FARS PROVINCE,” GEOSCIENCES, vol. 15, no. 57, pp. 40–53, 2005, [Online]. Available: https://sid.ir/paper/31645/en

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