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Petrology and Tectonic Setting of Volcanic Rocks in West and South West of Salafchegan, Qom, Iran

机译:萨拉达克(Salafchegan)西南岩石岩石岩石岩石景观

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In the west and south-west part of Salafchegan near Zavarian village in Iran (in central Iranian volcano plotonic belt), there are some volcanic rocks. Based on petrography and geochemistry findings, these volcanic rocks are Basalt, Andesite, Tracky-Andesite, Trackyte, Latite, Dacite. Tectono-magmatic diagram Y versus Zr shows the magmatic arc setting and Zr/TiO2 versus Ce/P2O5 diagram contrasts post colligenal magmatic arcs. The HFSE depletion in the MORB spider diagram shows significant volcanic arc magmatism. The high enrichment of Eu, Sr, Th, Rb, Cs, K (LFS elements) and Y, Zr, Hf shows negative anomaly and subduction tectonic setting. Based on MORB, Chondrite and primitive mantle spider diagrams, LREE have enriched to HREE in this area. The results of petrography, geochemistry and tectonic setting studies in this area, indicate that neogene magmatism occurred in post colligenal tectonic setting—subduction of Neo-thetise ocean under central Iranian plate in neogen era.
机译:在伊朗的Zavarian Village附近的西南和西南部(伊朗中部伊朗火山腰带),有一些火山岩。基于岩画和地球化学调查结果,这些火山岩是玄武岩,安德莱特,追踪的安捷利亚特,Trackyte,Latite,Dacite。 Tectono-Magmatic图Y与Zr显示岩浆电弧设置和Zr / TiO2与CE / P2O5图表对比后拼刀岩岩弧。 Morb蜘蛛图中的HFSE耗尽显示了显着的火山弧岩浆。 Eu,Sr,Th,Rb,Cs,K(LFS元素)和y,Zr,Hf的高富集显示阴性异常和俯冲构造设置。基于Morb,Chondrite和原始地幔蜘蛛图,LREE在这一领域富裕地富裕。该地区的岩画,地球化学和构造研究的结果表明,新生岩浆在伊朗中部地区时代的伊朗板块下的新老年海洋后的新生儿岩浆中发生。

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