Works matching IS 0950091X AND DT 2008 AND VI 20 AND IP 3
Results: 9
Trench-forearc interactions reflected in the sedimentary fill of Talara basin, northwest Peru.
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- Basin Research, 2008, v. 20, n. 3, p. 305, doi. 10.1111/j.1365-2117.2007.00346.x
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U–Pb zircon and <sup>40</sup>Ar–<sup>39</sup>Ar K-feldspar dating of syn-sedimentary volcanism of the Neoproterozoic Maricá Formation: constraining the age of foreland basin inception and inversion in the Camaquã Basin of southern Brazil
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- Basin Research, 2008, v. 20, n. 3, p. 359, doi. 10.1111/j.1365-2117.2007.00349.x
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Late Carboniferous foreland basin formation and Early Carboniferous stretching in Northwestern Europe: inferences from quantitative subsidence analyses in the Netherlands.
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- Basin Research, 2008, v. 20, n. 3, p. 377, doi. 10.1111/j.1365-2117.2008.00353.x
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Role of pore pressure generation in sediment transport within half-grabens.
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- Basin Research, 2008, v. 20, n. 3, p. 419, doi. 10.1111/j.1365-2117.2008.00357.x
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Giant submarine collapse of a carbonate platform at the Turonian–Coniacian transition: The Ayabacas Formation, southern Peru.
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- Basin Research, 2008, v. 20, n. 3, p. 333, doi. 10.1111/j.1365-2117.2008.00358.x
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Temporal constraints on basin inversion provided by 3D seismic and well data: a case study from the South Viking Graben, offshore Norway.
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- Basin Research, 2008, v. 20, n. 3, p. 397, doi. 10.1111/j.1365-2117.2008.00359.x
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‘LOSCS’ Lateral Offset Stacked Channel Simulations: Towards geometrical modelling of turbidite elementary channels.
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- Basin Research, 2008, v. 20, n. 3, p. 431, doi. 10.1111/j.1365-2117.2008.00361.x
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Morphology and distribution of Oligocene and Miocene pockmarks in the Danish North Sea – implications for bottom current activity and fluid migration.
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- Basin Research, 2008, v. 20, n. 3, p. 445, doi. 10.1111/j.1365-2117.2008.00362.x
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Pro- vs. retro-foreland basins.
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- Basin Research, 2008, v. 20, n. 3, p. 285, doi. 10.1111/j.1365-2117.2008.00366.x
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- Article