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Geologia do Corpo Intermediário/Máfico Umari, NW do Domínio Rio Piranhas-Seridó [PDF]
, 2019 The Ediacaran magmatism (~ 600 Ma) that occurred in the Rio Piranhas-Seridó Domain was aperiod of intense granitic plutonism, expressed in the form of plugs and batholiths, and was related to the formation of the paleocontinent Gondwana.
Tavares, Caio de Freitas
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