PETROGENESIS OF KUH E-DOM GRANITOID INTRUSION, NE ARDESTAN

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KANANIAN A.; SARJOUGHIAN F.; AHMADIAN J.; MIRNEZHAD H.

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Paper Information

Journal: JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT) Year:2008 | Volume:34 | Issue:2 Page(s): 41-53

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Information Journal Paper

Title

PETROGENESIS OF KUH E-DOM GRANITOID INTRUSION, NE ARDESTAN

Author(s)

KANANIAN A. | SARJOUGHIAN F. | AHMADIAN J. | MIRNEZHAD H. | Issue Writer Certificate

Keywords

HIGH POTASSIUM GRANITOIDQ3

I TYPEQ3

SUBDUCTIONQ2

KUH E-DOMQ3

Abstract

The KUH E-DOM intrusion is part of Urumieh- Dokhtar magmatism in Central Iran Zone. These rocks range from acidic (granodiorite, monzogranite, quartz monzonite) to intermediate (diorite, quartz diorite, monzodiorite and quartz monzodiorite) igneous rocks. The intermediate rocks occur as bands surrounding northern, southern and eastern margins of the acidic rocks. Based on field, petrographic and geochemical studies, Kuh e- Dom intrusion is I TYPE, high potassium calcalkaline and metaluminous. Chondrite and primitive mantle normalized trace element patterns for most of the sample show enrichment in LREE and LILE and pronounced negative anomalies in Eu, Ba, Nb, Ti, P and Sr. Such geochemical characteristics are typical of magmatism at active continental margin. High Potassium (~4.8%) and La (24 ppm) contents and enrichments in LILE and Pb along with negative HFSE and Ba anomalies indicate that the magma was probably generated by partial melting of lower crust.

Cites

EFFECTIVE PROCESSES IN EVOLUTION OF KUH-E DOM PLUTONISM, NE ARDESTAN, THE USING OF GEOCHEMICAL AND ISOTOPIC EVIDENCE

References

MINERAL CHEMISTRY AND THERMOBAROMETRY OF KUH E-DOM GRANITOID, NE ARDESTAN

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APA: Copy

KANANIAN, A., SARJOUGHIAN, F., AHMADIAN, J., & MIRNEZHAD, H.. (2008). PETROGENESIS OF KUH E-DOM GRANITOID INTRUSION, NE ARDESTAN. JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT), 34(2), 41-53. SID. https://sid.ir/paper/2213/en

Vancouver: Copy

KANANIAN A., SARJOUGHIAN F., AHMADIAN J., MIRNEZHAD H.. PETROGENESIS OF KUH E-DOM GRANITOID INTRUSION, NE ARDESTAN. JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT)[Internet]. 2008;34(2):41-53. Available from: https://sid.ir/paper/2213/en

IEEE: Copy

A. KANANIAN, F. SARJOUGHIAN, J. AHMADIAN, and H. MIRNEZHAD, “PETROGENESIS OF KUH E-DOM GRANITOID INTRUSION, NE ARDESTAN,” JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT), vol. 34, no. 2, pp. 41–53, 2008, [Online]. Available: https://sid.ir/paper/2213/en

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