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Cristian Rodrigo,Jenny M. Blamey,Oliver Huhn,Christine Provost     Pág. 344 - 356
The rifting zone of Bransfield Strait, Antarctica, is tectonically and geologically unique. It is a back-arc basin that was opened by extensional forces associated to roll-back subduction after cessation of spreading activity of the Phoenix Ridge, and th... ver más
Revista: Andean Geology    Formato: Electrónico

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