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作 者:Samira Bakhtiyari Mohammad Lotfi Nima Nezafati Arash Gourabjeripour Samira Bakhtiyari;Mohammad Lotfi;Nima Nezafati;Arash Gourabjeripour(Department of Geology, Science and Research Branch, Islamic Azad University, Tehran, Iran;Department of Geology, North Tehran Branch, Islamic Azad University, Tehran, Iran;Faculty of Natural Resources, Myianeh Branch, Islamic Azad University, Miyaneh, Iran)
机构地区:[1]Department of Geology, Science and Research Branch, Islamic Azad University, Tehran, Iran [2]Department of Geology, North Tehran Branch, Islamic Azad University, Tehran, Iran [3]Faculty of Natural Resources, Myianeh Branch, Islamic Azad University, Miyaneh, Iran
出 处:《Open Journal of Geology》2016年第12期1580-1590,共11页地质学期刊(英文)
摘 要:This paper presents an overview about the XIV iron-oxide prospect which is located in the Bafq mining district, central Iran. The prospect and its host rocks were investigated by field observations together with mineralogical and geochemical studies. According to these investigations, the XIV prospect is similar to Kiruna-type iron deposits and demonstrates a magmatic source for the ore forming processes with a metasomatic overprinting.This paper presents an overview about the XIV iron-oxide prospect which is located in the Bafq mining district, central Iran. The prospect and its host rocks were investigated by field observations together with mineralogical and geochemical studies. According to these investigations, the XIV prospect is similar to Kiruna-type iron deposits and demonstrates a magmatic source for the ore forming processes with a metasomatic overprinting.
关 键 词:MAGNETITE METASOMATISM Magmatic Iron Kiruna Central Iran
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