SOURCE AND TECTONIC SETTING OF ZARJEBOSTAN (NE OF QAZVIN) PALEOGENE VOLCANIC ROCKS USING REE AND HFSE ELEMENTS

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.

KALANTARI KIMIA; KANANIAN A.; ASIABANHA A.; ELIASI M.

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

Journal Paper

Paper Information

Journal: GEOSCIENCES Year:2008 | Volume:17 | Issue:68 Page(s): 140-149

Download Full-Text

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

Persian Verion

View:

1,066

Download:

Cites:

Information Journal Paper

Title

SOURCE AND TECTONIC SETTING OF ZARJEBOSTAN (NE OF QAZVIN) PALEOGENE VOLCANIC ROCKS USING REE AND HFSE ELEMENTS

Author(s)

KALANTARI KIMIA | KANANIAN A. | ASIABANHA A. | ELIASI M. | Issue Writer Certificate

Keywords

ANDESITEQ2

SUBDUCTIONQ2

ACTIVE CONTINENTAL MARGINQ2

ALBORZQ2

Abstract

Paleogene basic to intermediate lava flows of Central ALBORZ, in the northeast of Qazvin city (Zarjebostan), include trachy-ANDESITE, basaltic trachy-ANDESITE and basaltic ANDESITE. These volcanic rocks are high-K calc-alkaline rocks. Based on the high LILE/HFSE and LREE/HREE ratios and their similar composition to SUBDUCTION volcanic rock suites; it seems that they have formed in a SUBDUCTION zone. The SUBDUCTION process has little effect on the concentration of Zr, Ta, Hf, Sm, Tb, Nd, Eu and Y elements, while it has strong influence on concentration of Th, U and La elements. Due to high Ba/La, Ba/Ta and La/Ta ratios and low TiO2 content of lavas, they could be attributed to magmatic arc setting. Th/Yb vs. Ta/Yb diagrams and association of study suite with extensive volume of acidic tuffs, indicate that these rocks have been formed in an ACTIVE CONTINENTAL MARGIN.

Cites

No record.

References

MAGMATIC EVOLUTION IN THE STRATOID LAVA FLOWS OF NORTH-EAST ZARJEBOSTAN AREA, QAZVIN, IRAN

Cite

APA: Copy

KALANTARI, KIMIA, KANANIAN, A., ASIABANHA, A., & ELIASI, M.. (2008). SOURCE AND TECTONIC SETTING OF ZARJEBOSTAN (NE OF QAZVIN) PALEOGENE VOLCANIC ROCKS USING REE AND HFSE ELEMENTS. GEOSCIENCES, 17(68), 140-149. SID. https://sid.ir/paper/32395/en

Vancouver: Copy

KALANTARI KIMIA, KANANIAN A., ASIABANHA A., ELIASI M.. SOURCE AND TECTONIC SETTING OF ZARJEBOSTAN (NE OF QAZVIN) PALEOGENE VOLCANIC ROCKS USING REE AND HFSE ELEMENTS. GEOSCIENCES[Internet]. 2008;17(68):140-149. Available from: https://sid.ir/paper/32395/en

IEEE: Copy

KIMIA KALANTARI, A. KANANIAN, A. ASIABANHA, and M. ELIASI, “SOURCE AND TECTONIC SETTING OF ZARJEBOSTAN (NE OF QAZVIN) PALEOGENE VOLCANIC ROCKS USING REE AND HFSE ELEMENTS,” GEOSCIENCES, vol. 17, no. 68, pp. 140–149, 2008, [Online]. Available: https://sid.ir/paper/32395/en

Related Journal Papers