INVESTIGATIONS ON THE QAHR-ABAD FLUORITE DEPOSIT SOUTHEASTSAQQEZ, KURDISTAN PROVINCE, BASED ON REE DATA

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.

BARATI M.; AKBARPOUR A.; TALE FAZEL E.; TALAI B.; MOSLEHI M.

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

Journal Paper

Paper Information

Journal: GEOSCIENCES Year:2016 | Volume:25 | Issue:100 Page(s): 155-164

Download Full-Text

Persian Verion

View:

1,117

Download:

Cites:

Information Journal Paper

Title

INVESTIGATIONS ON THE QAHR-ABAD FLUORITE DEPOSIT SOUTHEASTSAQQEZ, KURDISTAN PROVINCE, BASED ON REE DATA

Author(s)

Keywords

QAHR-ABADQ2

FLUORITE DEPOSITQ1

FLUID INCLUSIONSQ1

SAQQEZQ2

KURDISTANQ2

Abstract

The QAHR-ABAD FLUORITE DEPOSIT is located ~58 km southeast of SAQQEZ city, KURDISTAN province. This deposit is developed as scatter lenses, veins, and veinlets (stockwork structure) within carbonate rocks. Violet, green and colorless fluorites are recognized. Quartz, dolomite, calcite and barite are gangues. REE geochemistry of the deposit shows that the REE content of the fluorites lies between 20.18 and 48.38 ppm. The relatively higher concentration of LREEs in violet and colorless fluorites suggests that they formed at the first stages of mineralization. Calculation of Eu anomalies indicates that the fluorites formed in an alkaline to neutral and to some extent oxidizing conditions because the Eu anomaly cover a narrow range around 1. Negative Ceanomaly also confirms the oxidizing conditions for mineralizing fluids. Finally, by the studies of REE geochemistry it can be concluded that the QAHR-ABAD FLUORITE DEPOSIT is a product of hydrothermal activity of epithermal type and the mineralizing fluids were of magmatic or a basin fossil fluids origin. Magmatic activities in this district, can explain the hydrothermal nature for the deposit.

Cites

No record.

References

No record.

Cite

APA: Copy

BARATI, M., AKBARPOUR, A., TALE FAZEL, E., TALAI, B., & MOSLEHI, M.. (2016). INVESTIGATIONS ON THE QAHR-ABAD FLUORITE DEPOSIT SOUTHEASTSAQQEZ, KURDISTAN PROVINCE, BASED ON REE DATA. GEOSCIENCES, 25(100), 155-164. SID. https://sid.ir/paper/31704/en

Vancouver: Copy

BARATI M., AKBARPOUR A., TALE FAZEL E., TALAI B., MOSLEHI M.. INVESTIGATIONS ON THE QAHR-ABAD FLUORITE DEPOSIT SOUTHEASTSAQQEZ, KURDISTAN PROVINCE, BASED ON REE DATA. GEOSCIENCES[Internet]. 2016;25(100):155-164. Available from: https://sid.ir/paper/31704/en

IEEE: Copy

M. BARATI, A. AKBARPOUR, E. TALE FAZEL, B. TALAI, and M. MOSLEHI, “INVESTIGATIONS ON THE QAHR-ABAD FLUORITE DEPOSIT SOUTHEASTSAQQEZ, KURDISTAN PROVINCE, BASED ON REE DATA,” GEOSCIENCES, vol. 25, no. 100, pp. 155–164, 2016, [Online]. Available: https://sid.ir/paper/31704/en

Related Journal Papers