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An empirical model reveals mineral and geochemical characteristics of ore zones in apatite deposits, highlighting concentration patterns.
An empirical model is proposed for ore zone of the late-magmatic complex apatite occurrence within anorthosite formation, which includes new elements of mineralogical, geochemical and petrophysical zonation. The middle and apical parts of orebodies are shown to contain the highest concentration of apatite and oxide ferro-titanium minerals.
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Vorobiev et al. (1991) studied this question.
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