Geology, mineralization, mineralogy and genesis of Pirgheshlagh Cu-Zn-Pb deposit, NW Zanjan

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.

ZOLFAGHARI M.; NABATIAN GH.; AZIMZADEH A.M.; HONARMAND M.; AZIZI P.

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

Journal Paper

Paper Information

Journal: GEOSCIENCES Year:2018 | Volume:27 | Issue:109 Page(s): 133-148

Download Full-Text

Persian Verion

View:

584

Download:

Cites:

Information Journal Paper

Title

Geology, mineralization, mineralogy and genesis of Pirgheshlagh Cu-Zn-Pb deposit, NW Zanjan

Author(s)

Keywords

Volcanogenic massive sulfideQ1

Central IranQ2

PirgheshlaghQ1

MahneshanQ2

ZanjanQ1

Abstract

Pirgheshlagh Cu-Zn-Pb deposit is located in the Central Iranian zone, north-east of the Mahneshan in the Zanjan province. The Kahar Formation with Precambrian age is the oldest Formation in the area which cutted by the granitic dykes. The Pirgheshlagh Cu-Zn-Pb mineralization occurred mainly as tabular-shape within the metamorphosed sandstones, meta-andesitic tuff, meta-crystal lithic tuff and meta-andesite rocks. Based on the field and microscopic studies, the main minerals consist of chalcopyrite, sphalerite, galena, pyrite, arsenopyrite and minor magnetite. The ore textures consist of disseminated, laminated, massive and veinlet which the veinlet texture is occurred mainly in the lower part of deposit. Secondary minerals such as smithsonite, cerrusite, chalcocite, covellite, malachite, azurite, goethite and lepidochrosite have formed during supergene processes. The main alterations in the Pirgheshlagh deposit include silicic, sericitic, chlorite and carbonate. The results of this study suggest that the Cu-Zn-Pb mineralization in the Pirgheshlagh deposit is a Besshi-type valcogenic massive sulfide (VMS) mineralization.

Cites

No record.

References

No record.

Cite

APA: Copy

ZOLFAGHARI, M., NABATIAN, GH., AZIMZADEH, A.M., HONARMAND, M., & AZIZI, P.. (2018). Geology, mineralization, mineralogy and genesis of Pirgheshlagh Cu-Zn-Pb deposit, NW Zanjan. GEOSCIENCES, 27(109 ), 133-148. SID. https://sid.ir/paper/32637/en

Vancouver: Copy

ZOLFAGHARI M., NABATIAN GH., AZIMZADEH A.M., HONARMAND M., AZIZI P.. Geology, mineralization, mineralogy and genesis of Pirgheshlagh Cu-Zn-Pb deposit, NW Zanjan. GEOSCIENCES[Internet]. 2018;27(109 ):133-148. Available from: https://sid.ir/paper/32637/en

IEEE: Copy

M. ZOLFAGHARI, GH. NABATIAN, A.M. AZIMZADEH, M. HONARMAND, and P. AZIZI, “Geology, mineralization, mineralogy and genesis of Pirgheshlagh Cu-Zn-Pb deposit, NW Zanjan,” GEOSCIENCES, vol. 27, no. 109 , pp. 133–148, 2018, [Online]. Available: https://sid.ir/paper/32637/en

Related Journal Papers