Copyright by Nysha Chaderton 2009 - The University of Texas at ...
Copyright by Nysha Chaderton 2009 - The University of Texas at ...
Copyright by Nysha Chaderton 2009 - The University of Texas at ...
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Chapter 5: Conclusions<br />
SEDIMENTATION AND HYDROCARBON EXPLORATION WITHIN FOREARC BASINS<br />
<strong>The</strong> study area is a classic forearc basin depositional setting. Hydrocarbons have<br />
been produced economically from some forearc basins such as Cook Inlet, Alaska (Bruhn<br />
et al., 2000; Clough et al., 2001), and the ancient Gre<strong>at</strong> Valley forearc basin in California<br />
(Rentschler, 1985; Vermeesch et al., 2006). In addition to conventional hydrocarbon<br />
production, there is thought to be up to 245 tcf <strong>of</strong> gas available in the unconventional<br />
resource <strong>of</strong> coal bed methane in Cook Inlet, Alaska (Clough et al., 2001; Montgomery<br />
and Barker, 2003).<br />
<strong>The</strong> re-interpret<strong>at</strong>ion <strong>of</strong> the Scotland Form<strong>at</strong>ion as a forearc basin deposit has<br />
implic<strong>at</strong>ions for hydrocarbon explor<strong>at</strong>ion onshore and <strong>of</strong>fshore Barbados. It has been<br />
accepted for several years th<strong>at</strong> the oil and gas production onshore Barbados is the only<br />
example <strong>of</strong> successful hydrocarbon production from true accretionary prism sediments.<br />
<strong>The</strong> new model presented in this research re-defines the depositional setting <strong>of</strong> the<br />
reservoirs and classifies them as forearc basin plays similar to Alaska or California.<br />
Sediment<strong>at</strong>ion within forearc basins is a combin<strong>at</strong>ion <strong>of</strong> deposition <strong>by</strong> turbidity<br />
currents travelling parallel to the volcanic arc along the basin axis or travelling<br />
perpendicular to the volcanic arc. In the case <strong>of</strong> island arcs, the sediment sources are<br />
usually localized to the volcanic islands (Moore et al., 1980). In the case <strong>of</strong> the Lesser<br />
Antilles volcaniclastic sediments are interbedded with the longitudinal input from the<br />
South American continent.<br />
Clastic sediments within the Tobago Forearc Basin (TFB) were transported<br />
parallel to the Lesser Antilles Island Arc as evidenced from seismic reflectors prograding<br />
from south to north and channels th<strong>at</strong> are visible in the strike (east to west) direction<br />
across the basin. Sediment input from the volcanic arc was minor, as evident from the<br />
small amounts <strong>of</strong> volcanic rock fragments th<strong>at</strong> have been identified in thin section.<br />
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