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anonymous,uncategorized,misc,general,other

However the occurrence of kaolinite in samples from Inca Huasi (1324) and San Manuel (0110) which do not belong to the height-temperature mineral assemblages might be either defined because of incomplete reactions to form pyrophyllite (+ diaspore) or, extra probably, as a late alteration part generated throughout waning temperatures of penetrating hydrothermal fluids.

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