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Precambrian Research, 2001
Abstract The Neoproterozoic Adamastor-Brazilide Ocean was generated during the breakup of the Rodinia supercontinent, and remnants of its oceanic lithosphere have been found in the Brasiliano-Pan African orogenic system that includes the Aracuai, West-Congo, Brasilia, Ribeira, Kaoko, Dom Feliciano, Damara and Gariep belts.
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Abstract The Neoproterozoic Adamastor-Brazilide Ocean was generated during the breakup of the Rodinia supercontinent, and remnants of its oceanic lithosphere have been found in the Brasiliano-Pan African orogenic system that includes the Aracuai, West-Congo, Brasilia, Ribeira, Kaoko, Dom Feliciano, Damara and Gariep belts.
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