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The Phanerozoic Tectonic and Sedimentary Evolution of North America
The Sedimentary Basins of the United States and Canada, 2019The Phanerozoic history of North America, when viewed from the perspective of Pangea, can be divided into three broad phases with gradational time boundaries, as described in the following paragraphs.
A. Miall, R. Blakey
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Developments in Structural Geology and Tectonics, 2019
Spatially widespread and extended periods of sedimentation coupled with distinct phases of tectonism resulted in complex stratigraphic relationships on the northeast margin of the Arabian Plate. The Mesozoic and Cenozoic strata were incorporated into the
Iraj Abdollahie-Fard +3 more
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Spatially widespread and extended periods of sedimentation coupled with distinct phases of tectonism resulted in complex stratigraphic relationships on the northeast margin of the Arabian Plate. The Mesozoic and Cenozoic strata were incorporated into the
Iraj Abdollahie-Fard +3 more
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Structural controls on sedimentary basin evolution: introduction
Tectonophysics, 1997This volume contains a collection of papers on structural controls on sedimentary basin evolution presented at the sixth annual workshop of the International Lithosphere Program Task Force 'Origin of Sedimentary Basins' in Sitges, at the rim of the Ebro Basin, September 1995. Previous workshops of the ILP Task Force had been in Rueil Malmaison, France (
S. Cloetingh +4 more
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Sedimentary Stratigraphy and Paleogeographic Evolution
1985Partsch (1887) introduced this name for the limestone of the Pantokrator mountain on Corfou island (Western Greece), Renz (1955) precised the stratigraphic range as Late Triassic to Early Jurassic and mentioned the similarity with the Late Triassic limestones of the Central Argolis Peninsula. Formally introduced by SuSskoch (1967) and later by Bannert &
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Plate Tectonic Evolution of Sedimentary Basins
1978The vertical tectonics inherent in the scheme of lateral motions of plates of lithosphere affords a coherent logic for the analysis of sedimentary basins. Subsidence may stem from crustal attenuation, thermotectonics, flexure of lithosphere, or combinations of these influences in space or time.
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Late Quaternary sedimentary evolution of the outer shelf of the East China Sea
Quaternary International, 2018This study investigated the late Quaternary sedimentary evolution of the outer shelf of the East China Sea (ECS) using borehole core data (DH02). Three unconformity-bounded sedimentary facies, namely, prodelta facies of marine isotopic stage (MIS) 3 ...
Taoyu Xu +13 more
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Sedimentary Geology, 2018
The break-up of Pangea remains one of the most interesting moments in the Earth's history. In the Pyrenees this geological moment is represented by continental successions, giving rise to a magnificent example of the creation of new basins and their ...
J. Lloret +6 more
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The break-up of Pangea remains one of the most interesting moments in the Earth's history. In the Pyrenees this geological moment is represented by continental successions, giving rise to a magnificent example of the creation of new basins and their ...
J. Lloret +6 more
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Marine and Petroleum Geology, 2018
The responses of depositional patterns to extensional faulting during the rift cycle are discussed in this article, based on an integrated analysis of 3D seismic reflections, wire logs and cores from the Early Cretaceous Tanan Depression in the Tamtsag ...
J. Ge +4 more
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The responses of depositional patterns to extensional faulting during the rift cycle are discussed in this article, based on an integrated analysis of 3D seismic reflections, wire logs and cores from the Early Cretaceous Tanan Depression in the Tamtsag ...
J. Ge +4 more
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Computer Simulation of Sedimentary Cover Evolution
1993A computer program has been developed for the mathematical simulation of the mechanical evolution of a sedimentary basin. It is designed for use in numerical experiments to study the impact of different velocity patterns at the base of the basin on the dynamics of the surface and inner boundaries, as well as for use in reconstructing the formation and ...
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On the geochemical evolution of sedimentary rocks
Chemical Geology, 1982The average major-element compositions of clastic sedimentary rock assemblages (i.e. carbonates, evaporites and iron formations not considered) for various times in earth history (Archean, Early Proterozoic, Late Proterozoic, Phanerozoic) are reported, based largely on the compilations of F.L. Schwab.
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