GEOLOGICAL-MINERALOGICAL CHARACTERISTICS AND TRACE-ELEMENTS GEOCHEMISTRY IN AGHADJARI BAUXITE DEPOSIT, SOUTH OF SHAHINDEZH, NW OF IRAN

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.

ABEDINI ALI; KALAGARI A.A.; HAJALILOU B.

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

Journal Paper

Paper Information

Journal: Iranian Journal of Crystallography and Mineralogy Year:2008 | Volume:16 | Issue:2 Page(s): 341-356

Download Full-Text

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

Persian Verion

View:

1,341

Download:

Cites:

Information Journal Paper

Title

GEOLOGICAL-MINERALOGICAL CHARACTERISTICS AND TRACE-ELEMENTS GEOCHEMISTRY IN AGHADJARI BAUXITE DEPOSIT, SOUTH OF SHAHINDEZH, NW OF IRAN

Author(s)

ABEDINI ALI | KALAGARI A.A. | HAJALILOU B. | Issue Writer Certificate

Keywords

BUAXITEQ2

IMMOBILE ELEMENTSQ3

LATERITIZATIONQ3

ADSORPTIONQ2

AGHADJARIQ3

SHAHINDEZHQ2

Abstract

Aghadjari bauxite deposit is located in ~15km south of SHAHINDEZH, West-Azarbaidjan province. This deposit was developed as stratiform lenses along the contact of Rutheh and Elika carbonate formations. Bauxitization processes led to the formation of boehmite, diaspore, kaolinite, pyrophyllite, illite, hematite, goethite, anatase, rutile, and quartz. Ferrugenization and deferrugenization mechanisms are two important factors controlling distribution of elements in this deposit. Mafic igneous rocks are the potential protolith. Obtained data show that elements such as Al, Ti, Fe, Zr, Hf, REE, and Nb moved down from the upper horizons to the lower parts of residual system by organic complexes during kaolinization processes. The carbonate bedrocks played dual roles in distribution of elements in this deposit. These rocks neutralized the acidic weathering solutions causing an increase in deposition of iron oxides and hydroxides which in turn due to their ADSORPTION capacity caused considerable concentration of Cr, Co, and LREE in lower parts of the bauxite horizon. On the other hand, the carbonates by forming stable ionic complexes with HREEs caused these elements to drain out of the residual system.

Cites

References

No record.

Cite

APA: Copy

ABEDINI, ALI, KALAGARI, A.A., & HAJALILOU, B.. (2008). GEOLOGICAL-MINERALOGICAL CHARACTERISTICS AND TRACE-ELEMENTS GEOCHEMISTRY IN AGHADJARI BAUXITE DEPOSIT, SOUTH OF SHAHINDEZH, NW OF IRAN. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 16(2), 341-356. SID. https://sid.ir/paper/4234/en

Vancouver: Copy

ABEDINI ALI, KALAGARI A.A., HAJALILOU B.. GEOLOGICAL-MINERALOGICAL CHARACTERISTICS AND TRACE-ELEMENTS GEOCHEMISTRY IN AGHADJARI BAUXITE DEPOSIT, SOUTH OF SHAHINDEZH, NW OF IRAN. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2008;16(2):341-356. Available from: https://sid.ir/paper/4234/en

IEEE: Copy

ALI ABEDINI, A.A. KALAGARI, and B. HAJALILOU, “GEOLOGICAL-MINERALOGICAL CHARACTERISTICS AND TRACE-ELEMENTS GEOCHEMISTRY IN AGHADJARI BAUXITE DEPOSIT, SOUTH OF SHAHINDEZH, NW OF IRAN,” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 16, no. 2, pp. 341–356, 2008, [Online]. Available: https://sid.ir/paper/4234/en

Related Journal Papers