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Title

INVESTIGATION OF PETROGENESIS AND TECTONOMAGMATIC SETTING OF IGNEOUS ROCKS IN THE GHASSEMABAD AREA (SOUTHWEST NEYSHABOUR)

Pages

  273-286

Abstract

 Ghassemabad area is located in 40km southwest of the Neyshabour, and is considered as a part of the Sabzevar structural zone. The composition of the Eocene volcanic rocks, are tracyandesite to dacite and composition of the Oligo-Miocene plutonic rocks is varied from alkali feldspar granite to gabrodiorite. Based on the geochemical diagrams, they show calc-alkaline and meta-aluminous nature belonging to I-TYPE granitoids. Based on the geochemical studies, tectonic setting of the Ghasemabad dahaneh intrusion is comparable to the volcanic arc granitoids (VAG). These bodies have been created in volcanic arc of subduction continental margins. On the basis of the geochemical data and field relations, they have been resulted from the contribution of melts from oceanic subducted crust and its above mantle wedge. Genereted magma underwent fractional crystallization and assimilation and contamination with the upper crust.

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    APA: Copy

    GHARABAGHI, HABIB, & MAZAHERI, SEYED AHMAD. (2015). INVESTIGATION OF PETROGENESIS AND TECTONOMAGMATIC SETTING OF IGNEOUS ROCKS IN THE GHASSEMABAD AREA (SOUTHWEST NEYSHABOUR). GEOCHEMISTRY, 3(4), 273-286. SID. https://sid.ir/paper/230889/en

    Vancouver: Copy

    GHARABAGHI HABIB, MAZAHERI SEYED AHMAD. INVESTIGATION OF PETROGENESIS AND TECTONOMAGMATIC SETTING OF IGNEOUS ROCKS IN THE GHASSEMABAD AREA (SOUTHWEST NEYSHABOUR). GEOCHEMISTRY[Internet]. 2015;3(4):273-286. Available from: https://sid.ir/paper/230889/en

    IEEE: Copy

    HABIB GHARABAGHI, and SEYED AHMAD MAZAHERI, “INVESTIGATION OF PETROGENESIS AND TECTONOMAGMATIC SETTING OF IGNEOUS ROCKS IN THE GHASSEMABAD AREA (SOUTHWEST NEYSHABOUR),” GEOCHEMISTRY, vol. 3, no. 4, pp. 273–286, 2015, [Online]. Available: https://sid.ir/paper/230889/en

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