INVISIBLE GOLD WITHIN SULFIDES FROM THE CHAH-BAGH GOLD DEPOSIT, MUTEH MINING DISTRICT

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.

KOUHESTANI HOSSEIN; RASTAD E.; RASHIDNEZHAD OMRAN N.A.

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

Seminar Paper

Paper Information

Seminar: SYMPOSIUM OF EARTH SCIENCES
Year:2006 | Issue:24

Download Full-Text

View:

146

Download:

Information Seminar Paper

Title

INVISIBLE GOLD WITHIN SULFIDES FROM THE CHAH-BAGH GOLD DEPOSIT, MUTEH MINING DISTRICT

Author(s)

KOUHESTANI HOSSEIN | RASTAD E. | RASHIDNEZHAD OMRAN N.A.

Keywords

Not Registered.

Abstract

Chah-Bagh gold deposit is located in central part of Sanandaj-Sirjan zone, in Muteh mining district. Gold mineralization occured in ductile to ductile-brittle shear zones and is comparable with orogenic gold deposits. Principle ore minerals observed in mineralized zones are pyrite, chalcopyrite, Cu-bearing arsenopyrite, covellite, digenite and silver. Silver commonly occurs as native Ag intimately associated with siliceous gangue (nearly 5 µm) and as invisible association with the sulfide minerals. The maximum concentration of invisible Ag content is present within chalcopyrites. Although gold is not present as native form in siliceous gangue and altered sulfide mineral margins, but the electron microprobe analysis found evidence of invisible gold association with the sulfide minerals. Two phase of gold mineralization occur in the Chah-Bagh area: 1- invisible gold association with coarse-grain sulfides (pyrite and chalcopyrite); 2- invisible gold (the main phase) association with gold-bearing fine-grain sulfides (gold-bearing pyrite and chalcopyrite). Evidently, the replacement and precipitation of gold is an integral part of hydrothermal alteration systems and is associated with sulfidization.

Cites

No record.

References

No record.

Cite

APA: Copy

KOUHESTANI, HOSSEIN, RASTAD, E., & RASHIDNEZHAD OMRAN, N.A.. (2006). INVISIBLE GOLD WITHIN SULFIDES FROM THE CHAH-BAGH GOLD DEPOSIT, MUTEH MINING DISTRICT. SYMPOSIUM OF EARTH SCIENCES. SID. https://sid.ir/paper/902928/en

Vancouver: Copy

KOUHESTANI HOSSEIN, RASTAD E., RASHIDNEZHAD OMRAN N.A.. INVISIBLE GOLD WITHIN SULFIDES FROM THE CHAH-BAGH GOLD DEPOSIT, MUTEH MINING DISTRICT. 2006. Available from: https://sid.ir/paper/902928/en

IEEE: Copy

HOSSEIN KOUHESTANI, E. RASTAD, and N.A. RASHIDNEZHAD OMRAN, “INVISIBLE GOLD WITHIN SULFIDES FROM THE CHAH-BAGH GOLD DEPOSIT, MUTEH MINING DISTRICT,” presented at the SYMPOSIUM OF EARTH SCIENCES. 2006, [Online]. Available: https://sid.ir/paper/902928/en

Related Journal Papers

No record.

Related Seminar Papers

No record.

Related Plans

No record.

Recommended Workshops