Mineralogy, Geochemistry, fluid inclusions of Karat iron Skarn deposit, Sangan, NE of 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.

Rahimy cheshmegachi Haniye; Yazdi Mohammad; Gholizadeh Kazem

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:2024 | Volume:32 | Issue:2 Page(s): 243-256

Download Full-Text

Persian Verion

View:

Download:

Cites:

Information Journal Paper

Title

Mineralogy, Geochemistry, fluid inclusions of Karat iron Skarn deposit, Sangan, NE of Iran

Author(s)

Rahimy cheshmegachi Haniye | Yazdi Mohammad | Gholizadeh Kazem | Issue Writer Certificate

Keywords

Geochemistry

Fluid inclusions

Skarn

Karat

Sangan

NE of Iran

Abstract

The Karat iron deposit is located in the vicinity of Sangan mining district, in the Northeast of Iran. The basement rocks of the Karat area include hornfels, metamorphosed limestone, marble, sandstone, siltstone and red shale with interlayers of marl, shale and marl, thick-layered red conglomerate and alluvial deposits. The intrusion of a granite batholith in the sedimentary units of the Karat iron deposit has led to the formation of iron deposits in the margin of this batholith. The most important ore minerals include magnetite, hematite, goethite, limonite and a small amount of sulfide minerals such as pyrite and chalcopyrite. Geochemical data indicate a strong correlation between the Ni, Mg, and V to Fe in mineralization zone, which indicates the magmatic origin of the Karat iron deposit. In order to investigate the characteristics of the ore-forming fluid of the Skarn Karat iron deposit Fluid inclusions of quartz veins were analyzed. The results show that fluids are mainly (L+V) type, low to medium salinity (4.48 to 16.42% NaCl) and the homogenization temperature of 200 to 390 degrees Celsius. Mineralogical, geochemical, and fluid-inclusion data show that the magmatics, meteoric and metamorphic fluids are responsible for Fe-mineralization in the Skarn and Isothermal mixing and surface fluid dilution are main evolution factors in mineralization fluids. It seems that the main phase of mineralization has been occurred during the retrograde stage Skarn.

Multimedia

No record.

Cites

No record.

References

No record.

Cite

Related Journal Papers

No record.

Related Seminar Papers

No record.

Related Plans