prompt a fit of these areas with the Tanzania-Mozambique region of Africa and suggest an intercontinental 'humite-epoch' in Gondwanaland coeval with the waning stages of Pan-African tectonothermal activity. Far from these humite-bearing marbles, orange clinohumites are preserved in Brasiliano marbles from Itaoca/Gironda area (ES--Brazil). Such observation leads to the fact that Pan-African/Brasiliano Orogeny was not just one of increasing charnockite and granite genesis, but one also of concomitant intense fluorinated, water-rich fluid activity, which was transcontinental through Gondwanaland in its scope. Taken together, humite-bearing marbles from Pan-African/Brasiliano belts from Gondwanaland keep the huge dimensions of the halogenated hydrothermal fluid activity around such 'humite-epoch'.
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