Works matching IS 0950091X AND DT 2009 AND VI 21 AND IP 5
Results: 16
Seismic analysis of clinoform depositional sequences and shelf-margin trajectories in Lower Cretaceous (Albian) strata, Alaska North Slope.
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- Basin Research, 2009, v. 21, n. 5, p. 644, doi. 10.1111/j.1365-2117.2008.00392.x
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Genesis of an over-thickened shoreface sandstone tongue: The Rannoch and Etive formations of the Middle Jurassic Brent delta, North Sea.
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- Basin Research, 2009, v. 21, n. 5, p. 620, doi. 10.1111/j.1365-2117.2009.00395.x
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Quantitative analysis of net-transgressive shoreline trajectories and stratigraphic architectures: mid-to-late Jurassic of the North Sea rift basin.
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- Basin Research, 2009, v. 21, n. 5, p. 528, doi. 10.1111/j.1365-2117.2009.00414.x
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Stratigraphic evolution of the upper slope and shelf edge in the Karoo Basin, South Africa.
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- Basin Research, 2009, v. 21, n. 5, p. 502, doi. 10.1111/j.1365-2117.2009.00409.x
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Trajectory analysis of the lower Brent Group (Jurassic), Northern North Sea: contrasting depositional patterns during the advance of a major deltaic system.
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- Basin Research, 2009, v. 21, n. 5, p. 559, doi. 10.1111/j.1365-2117.2009.00410.x
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Clinoform quantification for assessing the effects of external forcing on continental margin development.
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- Basin Research, 2009, v. 21, n. 5, p. 738, doi. 10.1111/j.1365-2117.2009.00411.x
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- Article
Clinoform migration patterns of a Late Miocene delta complex in the Danish Central Graben; implications for relative sea-level changes.
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- Basin Research, 2009, v. 21, n. 5, p. 704, doi. 10.1111/j.1365-2117.2009.00413.x
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Depositional architecture of a low-gradient ramp shelf in an epicontinental sea: the lower Cretaceous of Svalbard.
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- Basin Research, 2009, v. 21, n. 5, p. 655, doi. 10.1111/j.1365-2117.2009.00399.x
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Shoreline trajectories on a glacially influenced stable margin – insight from the Barents Sea Shelf, NW Russia.
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- Basin Research, 2009, v. 21, n. 5, p. 759, doi. 10.1111/j.1365-2117.2009.00418.x
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Influence of point-source sediment-supply on modern shelf-slope morphology: implications for interpretation of ancient shelf margins.
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- Basin Research, 2009, v. 21, n. 5, p. 484, doi. 10.1111/j.1365-2117.2009.00420.x
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Sedimentology and sequence stratigraphy of the middle Jurassic Tarbert Formation, Oseberg South area (northern North Sea).
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- Basin Research, 2009, v. 21, n. 5, p. 597, doi. 10.1111/j.1365-2117.2009.00421.x
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Detailed mapping of marine erosional surfaces and the geometry of clinoforms on seismic data: a tool to identify the thickest reservoir sand.
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- Basin Research, 2009, v. 21, n. 5, p. 721, doi. 10.1111/j.1365-2117.2009.00422.x
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Anatomy of the seaward steps and seaward termination of the Brent clastic wedge.
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- Basin Research, 2009, v. 21, n. 5, p. 573, doi. 10.1111/j.1365-2117.2009.00423.x
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Trajectory analysis: concepts and applications.
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- Basin Research, 2009, v. 21, n. 5, p. 454, doi. 10.1111/j.1365-2117.2009.00425.x
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Shelf edge and shoreline trajectories, a dynamic approach to stratigraphic analysis.
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- Basin Research, 2009, v. 21, n. 5, p. 445, doi. 10.1111/j.1365-2117.2009.00432.x
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Erosional vs. accretionary shelf margins: the influence of margin type on deepwater sedimentation: an example from the Porcupine Basin, offshore western Ireland.
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- Basin Research, 2009, v. 21, n. 5, p. 676, doi. 10.1111/j.1365-2117.2009.00424.x
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- Article