Abstract
Barrier island depositional systems are particularly challenging as exploration and development objectives because they span a very wide range of sizes and shapes depending on their tectonic setting and temporal position within a sea-level cycle. Sands in a barriered shoreline commonly grade along depositional strike into wave-dominated, sandy deltas and strand plains. Where rates of subsidence and sediment supply are high, such as on passive margins or on the thrustbelt sides of foreland basins for example, relative sea-level rise is accompanied by rapid shoreline aggradation, which results in thick, multistoried sand bodies with uniform strike orientations. Regional sandstone/shale ratios are often so high in these stacked intervals that trap integrity requires structural closure. Where subsidence rates are relatively low and the result is a single-story regressive sequence, preservation of even one entire barrier island can provide enough reservoir for a giant hydrocarbon accumulation.
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Barwis, J.H. (1990). Flood-Tidal Delta Reservoirs, Medora-Dickinson Trend, North Dakota. In: Barwis, J.H., McPherson, J.G., Studlick, J.R.J. (eds) Sandstone Petroleum Reservoirs. Casebooks in Earth Sciences. Springer, New York, NY. https://doi.org/10.1007/978-1-4613-8988-0_17
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