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首页> 外文期刊>CIM Bulletin >Geology and geochemistry of the Aguas Claras and Pico Iron mines, Iron Quadrangle, Minas Gerais, Brazil
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Geology and geochemistry of the Aguas Claras and Pico Iron mines, Iron Quadrangle, Minas Gerais, Brazil

机译:巴西米纳斯吉拉斯州铁四方铁矿Aguas Claras和Pico铁矿的地质和地球化学

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摘要

The Aguas Claras and Pico mines of Mineracoes Brasileiras Reunidas (MBR) are located in the Iron Quadrangle, Brazil, The orebodies of the Aguas Claras and Pico mines are hosted in itabirites (oxidized, metamorphosed, and heterogeneously deformed banded iron formation) of the Caue Formation, Itabira Group. Itabirites are very similar in lithology to most major oxide-facies banded iron formations (BIFs) known worldwide.
机译:Mineracoes Brasileiras Reunidas(MBR)的Aguas Claras和Pico矿山位于巴西的Iron Quadrangle,Acaus Claras和Pico矿的矿体寄居在Caue的艾铁矿(氧化,变质和异质变形带状铁矿)中。 Itabira集团成立。钛铁矿的岩性与全世界已知的大多数主要氧化物相带状铁形成物(BIF)十分相似。

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