Mineralogical, Geochemical and Genetic Aspects of Mineralization in Abgareh copper deposit; Typical vein-type Cu deposits

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.

Mahabady Raziyeh; Fardoost Farajollah

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

Journal Paper

Paper Information

Journal: GEOSCIENCES Year:2020 | Volume:29 | Issue:116 Page(s): 99-110

Download Full-Text

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

Persian Verion

View:

331

Download:

Cites:

Information Journal Paper

Title

Mineralogical, Geochemical and Genetic Aspects of Mineralization in Abgareh copper deposit; Typical vein-type Cu deposits

Author(s)

Mahabady Raziyeh | Fardoost Farajollah | Issue Writer Certificate

Keywords

MineralizationQ2

GeochemistryQ1

Fluid inclusionQ1

Vein-type CuQ1

AbgarehQ1

Abstract

Abgareh copper deposit located in 140 km southwest of shahrood and part of a volcanic-sedimentary Torud-Chah shirin belt that has facies in the northern edge Structural-sedimentary zones of Central Iran. Field and petrographical studies, deposit area, consist of andesite, basaltic andesite and basalt and contains less includes tuffit crystal that indicate middle– upper Eocene with with argillitic, sericitic, silicic, carbonatic, chloritic and iron oxides alterations. According to the field observations and mineralogical studies, the Mineralization in the region was carried out in two stages: hypogene and supergene and weathering. Hypogen zone minerals are generally pyrite, chalcopyrite and bornite. Because of existence in oxidizing-supergene environment, nearly almost Cu-bearing minerals of the main stage of Mineralization have been replaced by secondary Cu minerals such as chalcocite, covellite, malachite and chrysocolla. Fluid inclusion data shows in the temperature range from 145 to 217 ° C and salinity between 3. 73 and 9. 84 Wt%NaCl and depths less than 390 m. The host rocks, ore mineralogy, ore structures and textures, and Fluid inclusions characteristics and comparison with similar epithelial deposits indicate that the Abgareh vein system is formed in a low-sulfidation epitermal environment.

Cites

No record.

References

No record.

Cite

APA: Copy

Mahabady, Raziyeh, & Fardoost, Farajollah. (2020). Mineralogical, Geochemical and Genetic Aspects of Mineralization in Abgareh copper deposit; Typical vein-type Cu deposits. GEOSCIENCES, 29(116 ), 99-110. SID. https://sid.ir/paper/392185/en

Vancouver: Copy

Mahabady Raziyeh, Fardoost Farajollah. Mineralogical, Geochemical and Genetic Aspects of Mineralization in Abgareh copper deposit; Typical vein-type Cu deposits. GEOSCIENCES[Internet]. 2020;29(116 ):99-110. Available from: https://sid.ir/paper/392185/en

IEEE: Copy

Raziyeh Mahabady, and Farajollah Fardoost, “Mineralogical, Geochemical and Genetic Aspects of Mineralization in Abgareh copper deposit; Typical vein-type Cu deposits,” GEOSCIENCES, vol. 29, no. 116 , pp. 99–110, 2020, [Online]. Available: https://sid.ir/paper/392185/en

Related Journal Papers