Nohkuhi volcanogenic massive sulfide deposit: a sample of Bathurst-type mineralization in northwest of Kerman

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.

Pakizeh Sanajerdi A.; MOUSIVAND F.; RAJABI A.; MAGHFOURI S.

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

Journal Paper

Paper Information

Journal: GEOSCIENCES Year:2020 | Volume:29 | Issue:115 Page(s): 11-122

Download Full-Text

Persian Verion

View:

782

Download:

Cites:

Information Journal Paper

Title

Nohkuhi volcanogenic massive sulfide deposit: a sample of Bathurst-type mineralization in northwest of Kerman

Author(s)

Pakizeh Sanajerdi A. | MOUSIVAND F. | RAJABI A. | MAGHFOURI S. | Issue Writer Certificate

Keywords

Nohkuhi copper depositQ1

VMSQ1

Bathurst typeQ1

Posht-e-Badam blockQ1

Central IranQ2

Abstract

The Nohkuhi copper deposit located at 40 Km Northwest of Kerman, occurred in the Central Iran structural zone (Bafq-Posht-e-Badam block), within Late Precambrian-Early Cambrian volcano-sedimentary sequences. Host sequence of mineralization consists of dominantly black shale, sandstone and dacitic lava of Rizu Series. Mineralization occurred as stratabound (vein-veinlets) and stratiform (bedded) in the three copper-and two iron-manganese horizons. The mineralization in the Nohkuhi area involves four ore facieses including stringer, vent complex, bedded, and hydrothermal-exhalative banded iron and manganese-rich sediments. Ore textures are dominantly vein-veinlets, laminated, banded, massive, semi-massive, brecciated, and disseminated. This mineralization contains primary pyrite, chalcopyrite, sphalerite, hematite and pyrolusite, and secondary malachite, covelline, digenite, gypsum and Fe-Mn oxide and hydroxides. Gangue minerals are dominated by calcite, barite, quartz and chlorite. Wallrock alterations are dominated by chloritic and carbonatic-sericitic-silicic. Based on geochemistry of ore, metal zonation was observed in the deposit as enrichment of Cu in the stringer zone, and enrichment of Pb, Zn and Ag in the bedded facies. Considering the most important characteristics of mineralization at the Nohkuhi area, such as tectonic setting, host rocks, ore textures and structures, mineralogy, metal and alteration zonation, and comparison of the mineralization with main characters of the volcanogenic massive sulfide (VMS) deposits, the mineralization shows most similarities with the siliciclastic felsic or Bathurst-type deposits.

Cites

No record.

References

No record.

Cite

APA: Copy

Pakizeh Sanajerdi, A., MOUSIVAND, F., RAJABI, A., & MAGHFOURI, S.. (2020). Nohkuhi volcanogenic massive sulfide deposit: a sample of Bathurst-type mineralization in northwest of Kerman. GEOSCIENCES, 29(115 ), 11-122. SID. https://sid.ir/paper/378281/en

Vancouver: Copy

Pakizeh Sanajerdi A., MOUSIVAND F., RAJABI A., MAGHFOURI S.. Nohkuhi volcanogenic massive sulfide deposit: a sample of Bathurst-type mineralization in northwest of Kerman. GEOSCIENCES[Internet]. 2020;29(115 ):11-122. Available from: https://sid.ir/paper/378281/en

IEEE: Copy

A. Pakizeh Sanajerdi, F. MOUSIVAND, A. RAJABI, and S. MAGHFOURI, “Nohkuhi volcanogenic massive sulfide deposit: a sample of Bathurst-type mineralization in northwest of Kerman,” GEOSCIENCES, vol. 29, no. 115 , pp. 11–122, 2020, [Online]. Available: https://sid.ir/paper/378281/en

Related Journal Papers