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

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Figure 3.17: Photo <strong>of</strong> sample ITR 14 showing decreased plagioclase (pink) content. K<br />

feldspar (light brown and yellowish) and quartz grains are more abundant in this sample.<br />

......................................................................................................................................... 130<br />

Figure 3.18: Measured Section <strong>of</strong> outcrop CMRA showing the beds where sample<br />

CMRA was collected. ..................................................................................................... 131<br />

Figure 3.19: Photo <strong>of</strong> sample CMRA showing plagioclase (pink) and K-feldspar (light<br />

brown and yellowish) along with recycled quartz grains. Pore spaces are partially filled<br />

with grayish-brownish kaolinite cement......................................................................... 132<br />

Figure 3.20: Photo <strong>of</strong> sample from Breedy’s loc<strong>at</strong>ion (see Figure 2.8) showing<br />

plagioclase (pink) labeled plag, and K-feldspar (light brown and yellowish) labeled K..<br />

In the lower part <strong>of</strong> the photo there is a rounded, dark green grain th<strong>at</strong> is a glauconite<br />

grain. Volcanic rock fragments (VRF) are also present. ................................................ 132<br />

Figure 3.21: Composition <strong>of</strong> Scotland Form<strong>at</strong>ion samples point counted <strong>by</strong> Punch<br />

(2004), plotted on a QFR diagram. ................................................................................. 133<br />

Figure 3.22: Composition <strong>of</strong> Scotland Form<strong>at</strong>ion samples point counted <strong>by</strong> Kasper and<br />

Larue, (1986) plotted on a QFR diagram........................................................................ 133<br />

Figure 3. 23: Composition <strong>of</strong> Scotland Form<strong>at</strong>ion samples point counted in this study<br />

plotted on a QFR diagram............................................................................................... 134<br />

Figure 4.1: Base map showing seismic line survey and loc<strong>at</strong>ion <strong>of</strong> seismic lines used for<br />

interpret<strong>at</strong>ion in this study. Numbers indic<strong>at</strong>e lines shown in this paper. BB- Barbados<br />

Basin TFB- Tobago Forearc Basin, LAIA- Lesser Antilles Island Arc. ........................ 136<br />

Figure 4.2: Sedimentary units in outcrop and the seismic response <strong>of</strong> their <strong>of</strong>fshore<br />

equivalents ...................................................................................................................... 137<br />

Figure 4.3: Channels within Unit Five. <strong>The</strong> light blue horizon is the Middle Miocene<br />

unconformity th<strong>at</strong> bounds the top <strong>of</strong> Unit Four. ............................................................. 138<br />

Figure 4.4: East-west seismic reflection pr<strong>of</strong>ile showing the structural provinces within<br />

the study area. Oversized Pl<strong>at</strong>e (11x17) requires plotter or printer with tabloid printing.<br />

......................................................................................................................................... 139<br />

Figure 4.5: Seismic reflection pr<strong>of</strong>ile across the Barbados Ridge which shows the<br />

Barbados Fault to the east and the Tobago Forearc Basin sediments th<strong>at</strong> onlap the<br />

Barbados Accretionary Prism sediments to the west. <strong>The</strong> loc<strong>at</strong>ion <strong>of</strong> this seismic line is<br />

shown as line 2 in Figure 4.1. Oversized Pl<strong>at</strong>e (11x17) requires plotter or printer with<br />

tabloid printing................................................................................................................ 140<br />

......................................................................................................................................... 141<br />

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

......................................................................................................................................... 143<br />

Figure 4.9: Illustr<strong>at</strong>ion <strong>of</strong> the Speed model <strong>of</strong> tectonic emplacement <strong>of</strong> the Oceanic<br />

Form<strong>at</strong>ion (Tobago Forearc Basin sediments) onto accretionary prism sediments........ 144<br />

Figure 4.11: Illustr<strong>at</strong>ion <strong>of</strong> Hypothesis 2- early pelagic sediment<strong>at</strong>ion (Oceanic<br />

Equivalents) followed <strong>by</strong> clastic basin fill (Scotland Form<strong>at</strong>ion) and a return to pelagic<br />

sediment<strong>at</strong>ion (Oceanic Form<strong>at</strong>ion) th<strong>at</strong> is deposited conformably on the clastic basin fill.<br />

......................................................................................................................................... 146<br />

Figure A.1: Loc<strong>at</strong>ion map showing Scotland District Outcrops. Oversized Pl<strong>at</strong>e (11x17)<br />

requires plotter or printer with tabloid printing. ............................................................. 149<br />

Figure A.2a: Lidar Ridge measured section. .................................................................. 150<br />

xiv

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