Mineralogy and geochemical varations of altered host rock in Irankuh Pb-Zn mining district, SW Isfahan

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.

KARIMPOUR MOHAMMAD HASSAN; MALEKZADEH SHAFAROUDI AZADEH; ESMAEILI SEVIERI ABBAS; Shabani Saeed

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

Journal Paper

Paper Information

Journal: ADVANCED APPLIED GEOLOGY Year:2019 | Volume:8 | Issue:4 (30) Page(s): 1-16

Download Full-Text

Persian Verion

View:

532

Download:

Cites:

Information Journal Paper

Title

Mineralogy and geochemical varations of altered host rock in Irankuh Pb-Zn mining district, SW Isfahan

Author(s)

KARIMPOUR MOHAMMAD HASSAN | MALEKZADEH SHAFAROUDI AZADEH | ESMAEILI SEVIERI ABBAS | Shabani Saeed | Issue Writer Certificate

Keywords

MineralogyQ2

GeochemistryQ1

host rockQ2

Irankuh mining districtQ1

IsfahanQ2

Abstract

Irankuh Pb-Zn mining district is located Malayer-Isfahan Metallogenic Belt and it is MVT type. Mineralization is hosted by carbonate rock (mostly coarse-grained dolostone) and minor shale-siltstone as epigenetic. Mineral assembelages are sphalerite, galena, pyrite, and minor chalcopyrite associated with dolomite, ankerite, quartz, organic matter, calcite, and barite. Dolomitization is the most important alteration, which is occurred as karst and dissolution cavities filling, fossil replacement, veinlet, and fault berrecia cement. Silicification is mostly occurred at clastic host rock as vein-veinlet and open space fillinig. Geochemically, ore-bearing fluid is Fe-and Mn-rich, which is formed Fe-rich dolomite and ankerite at carbonate host rock. In clastic host rock, pyrite is mainly occurred due to reaction of iron of fluid and sulfur. In addition, As, Sb, Cd, and Cu contents of both carbonate and clastic host rocks are high that these elements can be exploratory tracker. This study in Irankuh mining district can be pattern of exploration for hidden sources in this area and similar deposits in Iran and the world.

Cites

No record.

References

No record.

Cite

APA: Copy

KARIMPOUR, MOHAMMAD HASSAN, MALEKZADEH SHAFAROUDI, AZADEH, ESMAEILI SEVIERI, ABBAS, & Shabani, Saeed. (2019). Mineralogy and geochemical varations of altered host rock in Irankuh Pb-Zn mining district, SW Isfahan. ADVANCED APPLIED GEOLOGY, 8(4 (30) ), 1-16. SID. https://sid.ir/paper/394515/en

Vancouver: Copy

KARIMPOUR MOHAMMAD HASSAN, MALEKZADEH SHAFAROUDI AZADEH, ESMAEILI SEVIERI ABBAS, Shabani Saeed. Mineralogy and geochemical varations of altered host rock in Irankuh Pb-Zn mining district, SW Isfahan. ADVANCED APPLIED GEOLOGY[Internet]. 2019;8(4 (30) ):1-16. Available from: https://sid.ir/paper/394515/en

IEEE: Copy

MOHAMMAD HASSAN KARIMPOUR, AZADEH MALEKZADEH SHAFAROUDI, ABBAS ESMAEILI SEVIERI, and Saeed Shabani, “Mineralogy and geochemical varations of altered host rock in Irankuh Pb-Zn mining district, SW Isfahan,” ADVANCED APPLIED GEOLOGY, vol. 8, no. 4 (30) , pp. 1–16, 2019, [Online]. Available: https://sid.ir/paper/394515/en

Related Journal Papers