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Tectono-metamorphic evolution of the internal zone of the Pan-African Lufilian orogenic belt (Zambia): Implications for crustal reworking and syn-orogenic uranium mineralizations
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文摘

P–T–td record of metamorphic rocks from the Pan-African Lufilian orogenic belt

D1 event at ca. > 550–530 Ma attributed to the syn-orogenic burial during continental subduction

D2 event at ca. 530–500 Ma interpreted to result from syn-orogenic exhumation of these HP units

Exhumation of the Lufilian root by development of a Metamorphic Core Complex

Regional U mineralizations at ca. 540–530 Ma synchronous to the syn-orogenic stage

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