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

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

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Figure 4.8: Isochron maps <strong>of</strong> the Lower Miocene to Plio-Pleistocene Tobago Basin fill. A. <strong>The</strong> Lower Miocene to Middle Miocene<br />

TFB fill is rel<strong>at</strong>ively thin. <strong>The</strong> thickest portion is preserved in the southwestern corner <strong>of</strong> the TFB. B. <strong>The</strong> Upper<br />

Miocene fill is almost identical in morphology to the underlying unit. <strong>The</strong> Pliocene to Pleistocene fill is concentr<strong>at</strong>ed in a<br />

narrow depocenter in the southwestern portion <strong>of</strong> the basin. <strong>The</strong> depocenter is constrained on its eastern margin <strong>by</strong> the<br />

Inner Forearc Deform<strong>at</strong>ion Front th<strong>at</strong> is shown in Figures 4.3 and 4.5. Seismic reflection pr<strong>of</strong>iles used to produce these<br />

isochron maps are loc<strong>at</strong>ed inside the green box in Figure 4.1.<br />

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