First Published: GEO ExPro, December 2019
Abstract
Mixed/hybrid deepwater turbiditic-contouritic depositional systems are only just beginning to be understood, but show great potential.
Several prolific discoveries have been associated with hybrid turbidite-contourite systems, of which the most notable is the Rovuma Basin offshore Mozambique (Maba Complex). Another significant hydrocarbon accumulation with clear seismic indications associated with a mixed system is the deepwater confined channel Barra/Moita Bonita complex (>3 Bbo in place) in the Sergipe Basin, Brazil.
Figure: (Sergipe) PSDM through a Barra well showing clear evidence for contourite drifts.
Identification of these systems relies on the recognition of a series of diagnostic criteria derived from the integration of available understanding (Sansom, 2018) and comparison with direct observations from well-established proven systems. Hydrocarbon potential evaluation includes the analysis of probable source rocks, reservoir and traps. Potential source rocks can be identified using a systematic frontier basin methodology which integrates plate tectonic reconstruction, paleographic setting, seismic character, any available well and outcrop data, and source rock characterization (Eastwell et al., 2018). To de-risk reservoir presence and quality, both depositional system features and seismic character can be used. The trapping mechanism is usually provided by the depositional characteristics of the hybrid system.
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