PETROGENESIS OF I-TYPE GRANITOIDS FROM THE KIKI BATHOLITH, NORTH-CENTRAL IRAN

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KAZEMI K.; KANANIAN A.; SARJOUGHIAN F.

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Journal: Iranian Journal of Geology Year:2013 | Volume:7 | Issue:25 Page(s): 49-63

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Title

PETROGENESIS OF I-TYPE GRANITOIDS FROM THE KIKI BATHOLITH, NORTH-CENTRAL IRAN

Author(s)

KAZEMI K. | KANANIAN A. | SARJOUGHIAN F. | Issue Writer Certificate

Keywords

BATHOLITHQ2

SUBDUCTIONQ2

CALC-ALKALINEQ2

CRUSTAL-MANTLE ORIGINQ2

I-TYPEQ2

Abstract

The Kiki BATHOLITH in the north Semnan Mountains of north-central Iran consists of granite, granodiorite, diorite, and gabbrodiorite sharply intruding Precambrian units. All rocks are met aluminous to slightly peraluminous, defining a calcalkalic trend. Rare earth element patterns indicate that all studied rock types are comagmatic. Mineralogic, petrographic, and major- and trace-element data demonstrate that all rocks are I-TYPE granitoids and crustal material along with derived mantle material may have contributed to their formation. Spider diagrams show troughs for Ti, P, and Nb, indicating magma genesis in a SUBDUCTIONzone setting. Other geochemical evidences such as high SiO2, low Mg# and transitional elements, and also Nb/La, Nb/Ce and (La/Sm) n average ratios indicate that the lower crust with derived mantle material had played an important role in generation of the Kiki granites.

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APA: Copy

KAZEMI, K., KANANIAN, A., & SARJOUGHIAN, F.. (2013). PETROGENESIS OF I-TYPE GRANITOIDS FROM THE KIKI BATHOLITH, NORTH-CENTRAL IRAN. IRANIAN JOURNAL OF GEOLOGY, 7(25), 49-63. SID. https://sid.ir/paper/129357/en

Vancouver: Copy

KAZEMI K., KANANIAN A., SARJOUGHIAN F.. PETROGENESIS OF I-TYPE GRANITOIDS FROM THE KIKI BATHOLITH, NORTH-CENTRAL IRAN. IRANIAN JOURNAL OF GEOLOGY[Internet]. 2013;7(25):49-63. Available from: https://sid.ir/paper/129357/en

IEEE: Copy

K. KAZEMI, A. KANANIAN, and F. SARJOUGHIAN, “PETROGENESIS OF I-TYPE GRANITOIDS FROM THE KIKI BATHOLITH, NORTH-CENTRAL IRAN,” IRANIAN JOURNAL OF GEOLOGY, vol. 7, no. 25, pp. 49–63, 2013, [Online]. Available: https://sid.ir/paper/129357/en

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