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Title

GEOCHEMISTRY, PETROGENESIS AND TECTONIC SETTING OF SAHAND SUBVOLCANIC AND VOLCANIC DOMES

Pages

  209-218

Keywords

HIGH SIO2 ADAKITEQ2

Abstract

 The Sahand volcano is located in the NW of Iran. Shand is a stratovolcano and is dominated by pyroclastic materials and lava flows of the Miocene-Quaternary. The last eruptions include subvolcanic and volcanic domes with dacitic to rhyolitic composition, which are studied in this paper as the YOUNG SAHAND. These rocks indicate petrological features including sieve texture and zoning in plagioclases. Common features in the young subvolcanic and volcanic rocks of the Sahand are abundance of plagioclase and amphibole, enrichment of Ba, Rb and Sr and negative Nb and Y anomalies in primitive mantle normalized multi-element diagrams and enrichment of LREE compared to HREE in chondrite-normalized REE patterns. These characteristics and the location of the rocks studied in the Y-Sr/Y diagram implying an adakitic composition for these rocks. The YOUNG SAHAND rocks are high SiO2 adakitic rocks. These rocks have been derived from partial melting of garnet-bearing crustal sources (thickened lower continental crust or oceanic crust) and underwent magmatic evolution during their ascent. The formation of studied rocks is related to the Arabian-Eurasia collision zone.

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    APA: Copy

    PIRMOHAMMADI ALISHAH, FARHAD. (2015). GEOCHEMISTRY, PETROGENESIS AND TECTONIC SETTING OF SAHAND SUBVOLCANIC AND VOLCANIC DOMES. GEOCHEMISTRY, 4(3), 209-218. SID. https://sid.ir/paper/230882/en

    Vancouver: Copy

    PIRMOHAMMADI ALISHAH FARHAD. GEOCHEMISTRY, PETROGENESIS AND TECTONIC SETTING OF SAHAND SUBVOLCANIC AND VOLCANIC DOMES. GEOCHEMISTRY[Internet]. 2015;4(3):209-218. Available from: https://sid.ir/paper/230882/en

    IEEE: Copy

    FARHAD PIRMOHAMMADI ALISHAH, “GEOCHEMISTRY, PETROGENESIS AND TECTONIC SETTING OF SAHAND SUBVOLCANIC AND VOLCANIC DOMES,” GEOCHEMISTRY, vol. 4, no. 3, pp. 209–218, 2015, [Online]. Available: https://sid.ir/paper/230882/en

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