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Copyright by Nysha Chaderton 2009 - The University of Texas at ...

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Sediment<strong>at</strong>ion within the Tobago Forearc Basin with implic<strong>at</strong>ions for<br />

the evolutionary history <strong>of</strong> the Southern Barbados Accretionary Margin<br />

Public<strong>at</strong>ion No._____________<br />

<strong>Nysha</strong> Alana Niela <strong>Chaderton</strong>, PhD<br />

<strong>The</strong> <strong>University</strong> <strong>of</strong> <strong>Texas</strong> <strong>at</strong> Austin, <strong>2009</strong><br />

Supervisor: Lesli J. Wood<br />

<strong>The</strong> Scotland Form<strong>at</strong>ion onshore Barbados is <strong>of</strong>ten called the only example <strong>of</strong> a<br />

successful hydrocarbon producing accretionary prism reservoir. In spite <strong>of</strong> this, the<br />

hydrocarbon system elements <strong>of</strong> the BAP have nevertheless not been well studied. Seven<br />

outcropping loc<strong>at</strong>ions <strong>of</strong> the Scotland were examined to document stacking p<strong>at</strong>terns, key<br />

surfaces, depositional element geometries, facies occurrences their vertical and l<strong>at</strong>eral<br />

extent, and the unit’s gamma response. Six facies were identified in outcrop: silty muds;<br />

lamin<strong>at</strong>ed, centimeter-scale sandstones interbedded with silts and muds; cross-str<strong>at</strong>ified<br />

sandstones; massive, medium to coarse-grained sandstones; very coarse grained sands<br />

with gravel or pebbles; and rare conglomer<strong>at</strong>es. <strong>The</strong>se facies combine to form<br />

architectural elements—channels, levees, and depositional lobes. Observ<strong>at</strong>ions from<br />

petrographic, outcrop and seismic d<strong>at</strong>a suggest th<strong>at</strong> the Scotland Form<strong>at</strong>ion was never<br />

deeply buried within the prism proper and was possibly deposited within the much larger<br />

proto-Tobago Basin.<br />

vi

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