【摘 要】
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The iron-oxide system can be used as a marker of oxidized and reduced conditions in closed systems. However, natural rocks with iron-oxide minerals also exhibit
【机 构】
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Federal University of Minas Gerais,Microscopy Center,Av.Ant nio Carlos 6627,Belo Horizonte,MG,Brazil
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The iron-oxide system can be used as a marker of oxidized and reduced conditions in closed systems. However, natural rocks with iron-oxide minerals also exhibit such reactions, although the natural system is typically open. To understand the behaviour of this natural system, they were investigated the similarities, in terms of crystallographic textures, between the microstructures of two systems: natural open system and synthetic closed system of iron-oxide phase transformation.
However, natural rocks with iron-oxide minerals also exhibit such reactions, although the natural system is typically open. To understand the behavior of this natural system , they were investigated the similarities, in terms of crystallographic textures, between the microstructures of two systems: natural open system and synthetic closed system of iron-oxide phase transformation.
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