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- W1873641998 abstract "Granitic magmatism related to the orogenic stages of the Aracuai Belt took place at 595-575 Ma, and are represented by two distinct suites. One is composed of I-type granitoids and includes the following plutons: Brasilândia (595±3 Ma), Sao Vitor (576±4 Ma) and Guarataia (574+2 Ma). The other suite comprises S-type granites like the Atalela (591±5 Ma) and Wolf (582±5 Ma) plutons. After a long period of magmatic quiescence, a batholith composed of the Caladao granite and Padre Paraiso charnockite intruded at 519±2 Ma. This magmatic episode is probably associated to the collapse of the orogen." @default.
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- W1873641998 date "2000-03-01" @default.
- W1873641998 modified "2023-09-23" @default.
- W1873641998 title "CHRONOLOGY OF NEOPROTEROZOIC-CAMBRIAN GRANITIC MAGMATISM IN THE ARAÇUAÍ BELT, EASTERN BRAZIL, BASED ON SINGLE ZIRCON EVAPORATION DATING" @default.
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- W1873641998 doi "https://doi.org/10.5327/rbg.v30i1.752" @default.
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