作者: Xiao-Wen Huang , Émilie Boutroy , Sheida Makvandi , Georges Beaudoin , Louise Corriveau
DOI: 10.1007/S00126-018-0825-1
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摘要: dc. description. abstract Trace element compositions of magnetite and hematite from 16 well-studied iron oxide–copper–gold (IOCG) and iron oxide apatite (IOA) deposits, combined with partial least squares-discriminant analysis (PLS-DA), were used to investigate the factors controlling the iron oxide chemistry and the links between the chemical composition of iron oxides and hydrothermal processes, as divided by alteration types and IOCG and IOA deposit subtypes. Chemical compositions of iron oxides are controlled by oxygen fugacity …