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A Moore, C. Finally, these fluids act as major markers of the geodynamic events that structure the basins and their mobilisation is directly governed by allocyclic parameters such as climate and sea-level variations. Next, between the onshore reservoirs, i. Lopez, H. Isolated seafloor pockmarks linked to BSRs, fluid chimneys, polygonal faults and stacked Oligocene-Miocene turbiditic palaeochannels in the Lower Congo Basin. A Gay, A. Seranne, D.

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