GEOCHEMISTRY, PETROLOGY AND GENESIS STUDY OF BAGHOO TURQUOISE DEPOSIT (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.

LIAGHAT S.; SHEYKHI V.; NAJARAN M.

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

Journal Paper

Paper Information

Journal: JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT) Year:2008 | Volume:34 | Issue:2 Page(s): 133-142

Download Full-Text

Persian Verion

View:

2,212

Download:

Cites:

Information Journal Paper

Title

GEOCHEMISTRY, PETROLOGY AND GENESIS STUDY OF BAGHOO TURQUOISE DEPOSIT (DAMGHAN)

Author(s)

LIAGHAT S. | SHEYKHI V. | NAJARAN M. | Issue Writer Certificate

Keywords

BAGHOOQ3

TURQUOISEQ3

GRANODIORITEQ3

DACITEQ3

ALUNITEQ3

IRANQ3

Abstract

The BAGHOO TURQUOISE deposit is hosted by Toroud- Chahshirin intrusive-volcanic belt (middle Eocene). Lithological units comprise andesite, rhyolite, GRANODIORITE and DACITE. The ore minerals occur as disseminated grains and veinlets in granodioritic to dacitic units. The ore minerals (Cu Al6 (PO4)4 (OH)8, 5H2O) range from 4mm to 1.2cm in thickness. The ore zone is limited by Anjiloo fault on the north and Toroud fault on the south. In order to achieve a genetic model for TURQUOISE deposition in the area, this study focuses on the structural observation made in the field, microscopy and geochemical analysis of ore minerals and host rock. Different types of fractures were analysed and the results indicate a good correlation with standard R, R’, P, T , Y type fractures. The TURQUOISE mineralization correlates with the strike of P group fractures. Microscopic studies of polished and thin sections indicate the presence of hypogene and supergene mineralization (oxidation and enrichment zone) in the area. Paragenetic sequence shows that hypogene zone includs pyrite, chalcopyrite and galena and oxidation zone includs iron hydroxide (goethite, hematite, and limonite), angelesite, cuprite, marchasite, azurite and malachite and enrichment zone contains covelite and chalcosite minerals. In addition, textural evidences show that TURQUOISE deposition has occurred in the waning stages of mineralization. Geochemical study confirms the results of IR, NAA, wet chemistry and SEM analysis and indicates that ALUNITE was gradually changed to TURQUOISE. A genetic model is presented for the formation of BAGHOO TURQUOISE.

Cites

No record.

References

No record.

Cite

APA: Copy

LIAGHAT, S., SHEYKHI, V., & NAJARAN, M.. (2008). GEOCHEMISTRY, PETROLOGY AND GENESIS STUDY OF BAGHOO TURQUOISE DEPOSIT (DAMGHAN). JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT), 34(2), 133-142. SID. https://sid.ir/paper/2200/en

Vancouver: Copy

LIAGHAT S., SHEYKHI V., NAJARAN M.. GEOCHEMISTRY, PETROLOGY AND GENESIS STUDY OF BAGHOO TURQUOISE DEPOSIT (DAMGHAN). JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT)[Internet]. 2008;34(2):133-142. Available from: https://sid.ir/paper/2200/en

IEEE: Copy

S. LIAGHAT, V. SHEYKHI, and M. NAJARAN, “GEOCHEMISTRY, PETROLOGY AND GENESIS STUDY OF BAGHOO TURQUOISE DEPOSIT (DAMGHAN),” JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT), vol. 34, no. 2, pp. 133–142, 2008, [Online]. Available: https://sid.ir/paper/2200/en

Related Journal Papers