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Title

GEOCHEMICAL CHARACTERISTICS OF ARDABIL AREA BASALTS

Pages

  4-11

Abstract

 Geochemistry of BASALTs were studied in three areas around ARDABIL including Heyran, Razei and Saein. Heyran and Razei are upper Cretaceous - lower Tertiary submarine PILLOW LAVA and Saein is the Quaternary aerial stair step (trapp) type. Heyran and Razei BASALTs are primitive with subcontinental LITHOSPHERIC MANTLE source and BASALT of Saein area is transitional with deeper source. According to isotopic ratio, 87Sr/86Sr belong to OIB array and based on isotopic ratio Nd-Sr is placed in mantle array and mean while it shows high CONTAMINATION with crust rocks.

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    APA: Copy

    DARVISHZADEH, ALI, & VASIGH, YOUSEF. (2012). GEOCHEMICAL CHARACTERISTICS OF ARDABIL AREA BASALTS. GEOCHEMISTRY, 1(1), 4-11. SID. https://sid.ir/paper/230842/en

    Vancouver: Copy

    DARVISHZADEH ALI, VASIGH YOUSEF. GEOCHEMICAL CHARACTERISTICS OF ARDABIL AREA BASALTS. GEOCHEMISTRY[Internet]. 2012;1(1):4-11. Available from: https://sid.ir/paper/230842/en

    IEEE: Copy

    ALI DARVISHZADEH, and YOUSEF VASIGH, “GEOCHEMICAL CHARACTERISTICS OF ARDABIL AREA BASALTS,” GEOCHEMISTRY, vol. 1, no. 1, pp. 4–11, 2012, [Online]. Available: https://sid.ir/paper/230842/en

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