PETROGEOCHEMISTRY OF THE SUNGUN PORPHYRY COPPER INTRUSIVE ROCKS, AZERBAIJAN, 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.

HEZARKHANIA A.

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

Journal Paper

Paper Information

Journal: AMIRKABIR Year:2004 | Volume:15 | Issue:59-D Page(s): 91-111

Download Full-Text

View:

279

Download:

Cites:

Information Journal Paper

Title

PETROGEOCHEMISTRY OF THE SUNGUN PORPHYRY COPPER INTRUSIVE ROCKS, AZERBAIJAN, IRAN

Author(s)

HEZARKHANIA A. | Issue Writer Certificate

Keywords

PETROGEOCHEMISTRY

COPPER

PORPHYRY

IRAN

Abstract

Based on the petrographical and petrochemical studies, it is suggested that the Sungun deposit as a composite stock, emplaced at a paleo-depth of ~2000 m, and comprising early monzonite/quartz- monzonite and a later diorite/granodiorite phase. The parental magma was a medium to high K andesite or diorite, initially contained >3 wt percent H2O (wet magma), and generated in continental arc settings. The high level emplacement of this magma, led to its saturation with water and the exsolution of fluids at an early stage of crystallization, and subsequently Mo and then Cu mineralization in the stock. Based on the major and trace element geochemistry, especially the behaviour of the immobile trace elements, Y, Zr and Nb, the fractional crystallization is suggested for the petrological characteristics of the present intrusive rocks. The degree of fractionation was estimated using a Rayleigh fractionation equation, which related the concentration of Zr, Nb and Y in the least altered sample to their concentrations in progressively more evolved samples. The results of these calculations indicated that the compositions of the various rock types can be explained by up to 24 % fractionation of a dioritic or andesitic magma to produce the more evolved monzonite/quartz-monzonite suite and chemically altered diorite-granodiorite suite.

Cites

No record.

References

No record.

Cite

APA: Copy

HEZARKHANIA, A.. (2004). PETROGEOCHEMISTRY OF THE SUNGUN PORPHYRY COPPER INTRUSIVE ROCKS, AZERBAIJAN, IRAN. AMIRKABIR, 15(59-D), 91-111. SID. https://sid.ir/paper/535636/en

Vancouver: Copy

HEZARKHANIA A.. PETROGEOCHEMISTRY OF THE SUNGUN PORPHYRY COPPER INTRUSIVE ROCKS, AZERBAIJAN, IRAN. AMIRKABIR[Internet]. 2004;15(59-D):91-111. Available from: https://sid.ir/paper/535636/en

IEEE: Copy

A. HEZARKHANIA, “PETROGEOCHEMISTRY OF THE SUNGUN PORPHYRY COPPER INTRUSIVE ROCKS, AZERBAIJAN, IRAN,” AMIRKABIR, vol. 15, no. 59-D, pp. 91–111, 2004, [Online]. Available: https://sid.ir/paper/535636/en

Related Journal Papers

No record.

Related Seminar Papers

No record.

Related Plans

No record.

Recommended Workshops