PETROLOGY OF SHOSHONITIC LAVAS IN SOUTH OF ASHIN VILLAGE (EAST OF ISFAHAN)

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NASR ESFAHANI A.KH.; AHMADI MAHMOUD

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Paper Information

Journal: JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY) Year:2008 | Volume:18 | Issue:69 (GEOLOGY ISSUE) Page(s): 89-98

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Information Journal Paper

Title

PETROLOGY OF SHOSHONITIC LAVAS IN SOUTH OF ASHIN VILLAGE (EAST OF ISFAHAN)

Author(s)

NASR ESFAHANI A.KH. | AHMADI MAHMOUD | Issue Writer Certificate

Keywords

PETROLOGYQ3

SHOSHONITIC LAVASQ3

ASHINQ3

UROMIA–DOKHTAR ZONEQ3

POSTCOLLISIONAL ARCQ3

IRANQ2

Abstract

Eocene felsic to basic SHOSHONITIC LAVAS are located in the Uromia-Dokhtoar structural zone. These association rocks are Absarokite, shoshonite, banakite and toscanite. PETROLOGY and geochemistery evidence indicate that the lavas were formed by fractionation of alkali basalt magma combined with assimilation of continental crust. Eruption of alkali basalt correlates with a POSTCOLLISIONAL ARC.

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APA: Copy

NASR ESFAHANI, A.KH., & AHMADI, MAHMOUD. (2008). PETROLOGY OF SHOSHONITIC LAVAS IN SOUTH OF ASHIN VILLAGE (EAST OF ISFAHAN). JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY), 18(69 (GEOLOGY ISSUE)), 89-98. SID. https://sid.ir/paper/70361/en

Vancouver: Copy

NASR ESFAHANI A.KH., AHMADI MAHMOUD. PETROLOGY OF SHOSHONITIC LAVAS IN SOUTH OF ASHIN VILLAGE (EAST OF ISFAHAN). JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY)[Internet]. 2008;18(69 (GEOLOGY ISSUE)):89-98. Available from: https://sid.ir/paper/70361/en

IEEE: Copy

A.KH. NASR ESFAHANI, and MAHMOUD AHMADI, “PETROLOGY OF SHOSHONITIC LAVAS IN SOUTH OF ASHIN VILLAGE (EAST OF ISFAHAN),” JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY), vol. 18, no. 69 (GEOLOGY ISSUE), pp. 89–98, 2008, [Online]. Available: https://sid.ir/paper/70361/en

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