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Petrology of Igneous Rocks in Northern Golpayegan, Iran
作者姓名:Mohammad  Ebrahimi
作者单位:Mohammad Ebrahimi Mohammad Reza HosseinNejad Faculty of Earth Sciences,China University of Geosciences,Wuhan 430074
基金项目:the University of Tehran,,
摘    要:INTRODUCTIONThestudiedareaislocatedinthenorthofGolpayegan,Iran,boundedbylatitudes33.31°Nand33.37°Nandlongi-tudes50.11°Eand50....

关 键 词:S-type  granite  volcanic  rocks  syenite

Petrology of Igneous Rocks in Northern Golpayegan, Iran
Mohammad Ebrahimi.Petrology of Igneous Rocks in Northern Golpayegan, Iran[J].Journal of China University of Geosciences,1998,9(1):2.
Authors:Mohammad Ebrahimi  Mohammad Reza HosseinNejad
Abstract:A preliminary study on petrological features of igneous rocks was carried out in northern Golpayegan, Iran, in an area of about 60 km 2. According to the limited available data the sequence of the magma activity could be considered as follows: (1) Precambrian (?) granite connected with a continental continental collision event, (2) Precambrian (?) syenite emplaced at a post continental continental collision environment, (3) Cretaceous volcanic rocks generated by a local extensional system at an active continental margin and (4) Cenozoic doleritic veins generated in a post collision event. Geochemical characteristics of the granitic intrusion show that it originated from crust and belongs to S type one. Syenitic body consists of syenitic affinities ranging from alkali syenite to syenodiorite. These rocks were cut by Cenozoic doleritic veins, which consist of dolerite and olivine dolerite. Both syenite and dolerite are thought to originate from upper mantle but their ages are different. Cretaceous volcanic rocks include basalt, andesite, trachyandesite, trachyte and tuff. They are compositionally alkaline and erupted in a shallow graben basin. Their eruption has been in connection with deep seated faults, which brought out the magma from the source.
Keywords:S-type granite  volcanic rocks  syenite  dolerite  Golpayegan  Iran
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