Presence of stratigraphic traps in the back arc basins of the southern shelf of Cuba
- Geophisical Enterprise, Havana (Cuba)
For the last ten years the southern shelf of Cuba has been the object of seismic investigations, mainly in the Ana Maria and Guacanayabo areas. More than 4000 km of seismic lines with 3000 % had been shot. These seismic surveys had confirmed the following geological events: (1) Presence of back arc extensional basins as a result of the ocean-ocean subduction. These basins started to form since Middle Cretaceous; (2) Presence of sedimentary sequences which change in thickness between 3.0-7.0 km; (3) Predominance of the extensional regime since Middle Cretaceous with subsidence, accommodation and extending of the sediments; (4) Development of stratigraphic traps, mainly associated with reef facies and slope fans of Late Cretaceous-Early Tertiary. These traps can reach some hundred square kilometers. They have very clear dynamic expression in the seismic section and usually form anomaly zones. Over these seismic anomalies some reverberation can be observed which could be related to hydrocarbon flows. The depth of the traps changes between 1.5-3.5 km. More than thirty of them have been localized; (5) Probably a wrench tectonic interested these basins since Middle Eocene; (6) in some wells has been found oil and gas seeps as well as seal sequences; (7) According to their origin and evolution they can be similar to the great oil basins of the Venezuela and Colombia.
- OSTI ID:
- 411904
- Report Number(s):
- CONF-9610180-; ISSN 0149-1423; TRN: 96:005901-0036
- Journal Information:
- AAPG Bulletin, Vol. 80, Issue 9; Conference: American Association of Petroleum Geologists (AAPG) gulf coast association of geological societies meeting, San Antonio, TX (United States), 2-4 Oct 1996; Other Information: PBD: Sep 1996
- Country of Publication:
- United States
- Language:
- English
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