GEOLOGY, MINERALOGY AND FLUID INCLUSION INVESTIGATION OF SUPERGENE ZN DEPOSIT IN KHARENGUN ZONE, NORTHEAST OF BAFQ, CENTRAL IRAN

Q: How can I download an article?

To download an article from SID, first log in to the site, search for the article title, and click on the 'Download Article' option.

Q: How can I download an ISI article?

To download an ISI article on SID, enter the keyword or article title in the search bar, view the relevant results, click on the desired article, and select the 'Download Article' option.

Q: How can I access the SID database?

To access the SID database, visit SID.ir, create an account, and log in to access scientific resources.

Q: Is downloading articles from SID free?

Some articles on SID are available for free, while others require payment. Details are specified on the article's page.

MIRIYAN Z.; LOTFI M.; SHABANI A.A.; MOKHTARI M.A.A.; HAJ MOLLA ALI E.

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Journal Paper

Paper Information

Journal: GEOSCIENCES Year:2015 | Volume:24 | Issue:95 (PETROLOGY & MINERALOGY) Page(s): 233-242

Download Full-Text

Persian Verion

View:

1,098

Download:

Cites:

Information Journal Paper

Title

GEOLOGY, MINERALOGY AND FLUID INCLUSION INVESTIGATION OF SUPERGENE ZN DEPOSIT IN KHARENGUN ZONE, NORTHEAST OF BAFQ, CENTRAL IRAN

Author(s)

Keywords

BAFQQ2

KHRENGUNQ2

SUPERGENEQ2

NONSULFIDE ZINCQ2

SMITHSONITEQ3

HEMIMORPHITEQ1

EPITHERMALQ3

Abstract

The Kharengun area is located in the Yazd province, Central Iran, 130 km east of Yazd city and 65 km northeast of BAFQ city. Mineralization in Kharengun area occurred within calcic and dolomitic units of the Rizou Formation (equivalent to Soltaniyeh Formation) of upper Precambrian- lower Cambrian age. The ore minerals of this deposit includes SMITHSONITE and HEMIMORPHITE, that is stratabound and formed epigenetically along layers and laminations of carbonate host rocks. The maximum grade of zinc in samples taken from the study area exceeds 36% and geochemical studies indicate significant absence of Pb along with Zn in this area. Therefore, the Kharengun mineralization is a monomineral Zn zone. The fluid inclusion microthermometry investments explain the role of meteoric waters in generation of this deposit. The homogenization temperatures and salinity of the inclusions show the similarity between these fluids and the solutions responsible for the development of EPITHERMAL deposits. The Zn mineralization present in this zone belongs to the nonsulfide SUPERGENE deposit class, and a mixture of wallrock replacement and direct replacement subclasses.

Cites

No record.

References

No record.

Cite

APA: Copy

MIRIYAN, Z., LOTFI, M., SHABANI, A.A., MOKHTARI, M.A.A., & HAJ MOLLA ALI, E.. (2015). GEOLOGY, MINERALOGY AND FLUID INCLUSION INVESTIGATION OF SUPERGENE ZN DEPOSIT IN KHARENGUN ZONE, NORTHEAST OF BAFQ, CENTRAL IRAN. GEOSCIENCES, 24(95 (PETROLOGY & MINERALOGY)), 233-242. SID. https://sid.ir/paper/31742/en

Vancouver: Copy

MIRIYAN Z., LOTFI M., SHABANI A.A., MOKHTARI M.A.A., HAJ MOLLA ALI E.. GEOLOGY, MINERALOGY AND FLUID INCLUSION INVESTIGATION OF SUPERGENE ZN DEPOSIT IN KHARENGUN ZONE, NORTHEAST OF BAFQ, CENTRAL IRAN. GEOSCIENCES[Internet]. 2015;24(95 (PETROLOGY & MINERALOGY)):233-242. Available from: https://sid.ir/paper/31742/en

IEEE: Copy

Z. MIRIYAN, M. LOTFI, A.A. SHABANI, M.A.A. MOKHTARI, and E. HAJ MOLLA ALI, “GEOLOGY, MINERALOGY AND FLUID INCLUSION INVESTIGATION OF SUPERGENE ZN DEPOSIT IN KHARENGUN ZONE, NORTHEAST OF BAFQ, CENTRAL IRAN,” GEOSCIENCES, vol. 24, no. 95 (PETROLOGY & MINERALOGY), pp. 233–242, 2015, [Online]. Available: https://sid.ir/paper/31742/en

Related Journal Papers