Abstract:The Panxi region, SW China, has been an important source of Fe, Ti, and V metals in the world. Several giant deposits, such as the Panzhihua, Hongge, Baima and Taihe, are hosted in ca. 260 Ma mafic-ultramafic layered intrusions in this region. These Fe-Ti oxide-bearing intrusions are unique in that they contain large proportions of massive ores in the lower and middle parts within the relatively small bodies. It is generally acknowledged that they have Fe-Ti-rich and Si-poor parental magmas that were derived f… Show more
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