RELATION OF GOLD MINERALIZATION WITH TECTONIC AND FAULT STRUCTURES OF GANDIAREA (SOUTH OF DAMGHAN)

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.

REZAEESHAHZADEH ZAHRA; BOUZARI SOHEILA; BADAKHSHANMOMTAZ GHEYS

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

Journal Paper

Paper Information

Journal: JOURNAL OF THE EARTH Year:2012 | Volume:6 | Issue:22 Page(s): 107-114

Download Full-Text

Persian Verion

View:

1,886

Download:

Cites:

Information Journal Paper

Title

RELATION OF GOLD MINERALIZATION WITH TECTONIC AND FAULT STRUCTURES OF GANDIAREA (SOUTH OF DAMGHAN)

Author(s)

REZAEESHAHZADEH ZAHRA | BOUZARI SOHEILA | BADAKHSHANMOMTAZ GHEYS | Issue Writer Certificate

Keywords

GOLD DEPOSITQ2

TOROUD FAULTQ3

ANJILOU FAULTQ2

MINERALIZAIONQ2

Abstract

The Gandi GOLD DEPOSIT is located in 130km South East of Damghan city and 25km North East of Moalleman village. The area is part of central Iran structural zone which is limited between two major fault, Anjilou in North and Toroud in South. Gandi GOLD DEPOSIThave 337453.68ton ore with 5.18ppm gold grad, and wholly 1.69ton gold estimated for it. The rock host consist of alteration of tuff, sandy tuff, siltstone and marl with upper Eocene age which is thin bedded in lower parts and medium to thick bedded in upper parts. Northword, An East-West fault zone separated Gandi deposit from volcanic and pyroclastic rock with andesite, basalt and dacite component. The major fault system of the area have NE-SW trend and trends of NW-SE and E-W have miner preference. Due to infusion of hydrothermal solution in the faults and fractures of the area, mineralized veins are formed and host rocks are altered (kaolinitization, silicification and jarositization). Mostly, the mineralized vein trended NE-SW and they have carbonit-silica and brecciated ore, with Fe oxides in the syrface. Gold has seen as a free metal in the ore and also as onclosion in the sulfide minerals and as petzit mineral (mineral consists of Te, Ag and Au) in this area (Badakhshanmomtaz 2003). Sub intrusive activities are known as the responsible for the gnesis of this mineralization (Ford 2002, Goliyaee 2000).

Cites

No record.

References

No record.

Cite

APA: Copy

REZAEESHAHZADEH, ZAHRA, BOUZARI, SOHEILA, & BADAKHSHANMOMTAZ, GHEYS. (2012). RELATION OF GOLD MINERALIZATION WITH TECTONIC AND FAULT STRUCTURES OF GANDIAREA (SOUTH OF DAMGHAN). JOURNAL OF THE EARTH, 6(22), 107-114. SID. https://sid.ir/paper/192919/en

Vancouver: Copy

REZAEESHAHZADEH ZAHRA, BOUZARI SOHEILA, BADAKHSHANMOMTAZ GHEYS. RELATION OF GOLD MINERALIZATION WITH TECTONIC AND FAULT STRUCTURES OF GANDIAREA (SOUTH OF DAMGHAN). JOURNAL OF THE EARTH[Internet]. 2012;6(22):107-114. Available from: https://sid.ir/paper/192919/en

IEEE: Copy

ZAHRA REZAEESHAHZADEH, SOHEILA BOUZARI, and GHEYS BADAKHSHANMOMTAZ, “RELATION OF GOLD MINERALIZATION WITH TECTONIC AND FAULT STRUCTURES OF GANDIAREA (SOUTH OF DAMGHAN),” JOURNAL OF THE EARTH, vol. 6, no. 22, pp. 107–114, 2012, [Online]. Available: https://sid.ir/paper/192919/en

Related Journal Papers