MINERALOGY AND TEXTURAL STUDIES OF MEHDIABAD ZINC-LEAD DEPOSIT- YAZD, 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.

GHASEMI MAHMOUD; MOUMENZADEH M.; YAGHOUBPOUR A.A.M.; MIRSHOKRAEI A.A.

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

Journal Paper

Paper Information

Journal: Iranian Journal of Crystallography and Mineralogy Year:2008 | Volume:16 | Issue:3 Page(s): 389-404

Download Full-Text

Persian Verion

View:

2,944

Download:

Cites:

Information Journal Paper

Title

MINERALOGY AND TEXTURAL STUDIES OF MEHDIABAD ZINC-LEAD DEPOSIT- YAZD, CENTRAL IRAN

Author(s)

GHASEMI MAHMOUD | MOUMENZADEH M. | YAGHOUBPOUR A.A.M. | MIRSHOKRAEI A.A. | Issue Writer Certificate

Keywords

MEHDIABADQ2

LOWER CREATACEOUSQ2

ZINC & LEADQ3

IRANQ2

TAPPEH SIAH FAULTQ3

Abstract

MEHDIABAD Zn-Pb-Ba deposit is located 110km south-east of Yazd, in the Central IRAN structural zone. The stratigraphic succession consists of three sedimentary formations of LOWER CREATACEOUS age. The Sangestan formation,i.e, the lowest unit of shale and siltstone with calcarenitic interbeded layers. This unit is overlain by ankeritic massive dolomite and dolomitic limestone of Taft formation. The Abkouh formation at the top is composed of cherty or clayey limestone with conglomeretic intercalation, lenses of massive reef limestone and calcareous shale. The structure of orebody shows a half-graben with a vast N-S synform being complicated by the presence of polyphase faults. The main normal fault is TAPPEH SIAH FAULT, suggested to have been active during and after the period of sedimentation. Major economic minerals are sphalerite, galena and barite with minor pyrite, chalchopyrite in sulfide zone. Oxide ores contain smithzonite, hydrozincite, hemimorphite and cerussite. Mineralization occurs in stratiform-lenticular orebodies and concordant with host rocks. Also orebodies showing laminated, disseminated, open space filling, karst filling, colloform and botryoidal textures.

Cites

EPIGENETIC DOLOMITIZATION AS AN EXPLORATION KEY FOR NON-SULFIDIC ZN-PB DEPOSITS WITH CARBONATE HOST ROCKS, CASE STUDY: CHAH-TALKH DEPOSIT (SIRJAN)

References

No record.

Cite

APA: Copy

GHASEMI, MAHMOUD, MOUMENZADEH, M., YAGHOUBPOUR, A.A.M., & MIRSHOKRAEI, A.A.. (2008). MINERALOGY AND TEXTURAL STUDIES OF MEHDIABAD ZINC-LEAD DEPOSIT- YAZD, CENTRAL IRAN. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 16(3), 389-404. SID. https://sid.ir/paper/4028/en

Vancouver: Copy

GHASEMI MAHMOUD, MOUMENZADEH M., YAGHOUBPOUR A.A.M., MIRSHOKRAEI A.A.. MINERALOGY AND TEXTURAL STUDIES OF MEHDIABAD ZINC-LEAD DEPOSIT- YAZD, CENTRAL IRAN. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2008;16(3):389-404. Available from: https://sid.ir/paper/4028/en

IEEE: Copy

MAHMOUD GHASEMI, M. MOUMENZADEH, A.A.M. YAGHOUBPOUR, and A.A. MIRSHOKRAEI, “MINERALOGY AND TEXTURAL STUDIES OF MEHDIABAD ZINC-LEAD DEPOSIT- YAZD, CENTRAL IRAN,” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 16, no. 3, pp. 389–404, 2008, [Online]. Available: https://sid.ir/paper/4028/en

Related Journal Papers