ALTERATION, MINERALIZATION AND GENESIS OF TUZLAR GOLD D

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.

RABIEI AHMAD; KOUSARI S.; HOSSEIN MASOUD

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:

270

Download:

Information Seminar Paper

Title

ALTERATION, MINERALIZATION AND GENESIS OF TUZLAR GOLD D

Author(s)

RABIEI AHMAD | KOUSARI S. | HOSSEIN MASOUD

Keywords

Not Registered.

Abstract

The host rock of mineralization within the deposit is a part of Sanandaj-Sirjan, Oligo-miocene age. The composition of these rocks is mainly from moderate to basic volcanic units of porphyritic pyroxene andesite that approximately has covered most of the area. The geological sequence of the locality is cut by some stocks and diabasic dykes. Tree zones of alteration were detected from TM satellite images with W-E elongation in area including silisification, prophilitic,phillic, Argillic, quartz-calsedonit-Alunite and advanced argillic alteration. The mineralization displays alteration pattern consisting of a core of residual (vuggy) silica, bordered outward by zones of quartz-kaolinite, alunite and montmorillonite. Some veins have occurred in alteration zones including gold-copper bearing veins in the west area and silver and base metals bearing veins in the middle area. Mineralization studies of alteration in the west area around silica veins by XRD indicated association of quartz, kaolonite, alunite, montmorillonite, jarosite, anatase. Mineralization studies on polished samples of silica veins by optical microscope and scanning electron microscope have showed anatase, tree generation of pyrite, enargite, tenantite, native gold, electrum with some barite and chromium minerals. The composition of veins varied in different veins. The veins are formed of vuggy silica which the vuggs (usually 5-20µm) hosted gold bearing third generation thin pyrite. Oxidation of the sulfides extricated gold in to secondary residual limonite. The type of mineralization, alteration, textures and situation of deposit forming in relation to intrusion bodies shows similarity to an epithermal high sulfidation deposit type with variation of mineralization in veins.

Cites

No record.

References

No record.

Cite

APA: Copy

RABIEI, AHMAD, KOUSARI, S., & HOSSEIN, MASOUD. (2006). ALTERATION, MINERALIZATION AND GENESIS OF TUZLAR GOLD D. SYMPOSIUM OF EARTH SCIENCES. SID. https://sid.ir/paper/902907/en

Vancouver: Copy

RABIEI AHMAD, KOUSARI S., HOSSEIN MASOUD. ALTERATION, MINERALIZATION AND GENESIS OF TUZLAR GOLD D. 2006. Available from: https://sid.ir/paper/902907/en

IEEE: Copy

AHMAD RABIEI, S. KOUSARI, and MASOUD HOSSEIN, “ALTERATION, MINERALIZATION AND GENESIS OF TUZLAR GOLD D,” presented at the SYMPOSIUM OF EARTH SCIENCES. 2006, [Online]. Available: https://sid.ir/paper/902907/en

Related Journal Papers

No record.

Related Seminar Papers

No record.

Related Plans

No record.

Recommended Workshops