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• W1520171873 abstract "The distribution of Upper Jurassic sandstones in the Central North Sea Basin was influenced by three structural mechanisms: (1) the contemporaneously evolving Central Graben rift system that formed the basin and created fault block highs and basinal grabens; (2) the movement of Zechstein salt (late Permian age) which can be locally very thick and (3) bathymetric features controlled by the Jurassic deformation of Triassic pods (salt minibasins). Rift development involved movement on deep seated, normal faults with offset seen at Rotliegend level (Permian). Zechstein salt decouples this fault displacement from the deformation of younger strata. As a result of the individual or combined effects of footwall uplift, salt movement or grounding of pods on the underlying Rotliegend, areas of former Triassic or Upper Jurassic deposition were subsequently reworked erosively and redistributed. It has been found that spiculitic sandstone layers within Upper Jurassic Fulmar Formation sandstones serve as useful horizons for correlation and help highlight intra-Jurassic erosive truncation of shoreface sandstones. Erosion of structurally controlled highs can result in reworking of earlier deposited shoreface sandstones, the products of this erosion being sometimes re-deposited as turbidites that are transported short distances before being ponded in depositional lows such as the hangingwall of major faults. The development of significant erosion surfaces within Upper Jurassic shallow marine sandstones is linked to tectonic mechanisms. It is probable that these surfaces are not basin wide sequence boundaries; rather they are local surfaces reflecting the dynamic and geographically varied evolution of the basin. Previous proposals that many phases of incised valley development occurred during the Late Jurassic generating 3rd order sequence boundaries do not appear to be backed by sedimentary evidence. While turbidite sandstones are evidently developed at various times in the basin history, their relationship to proximal fluvial systems and incised valleys is unproven. A preferred interpretation is that local tectonic uplift and shoreface erosion are the main mechanisms for redistributing Jurassic and older sediments." @default.
• W1520171873 created "2016-06-24" @default.
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• W1520171873 date "2014-08-01" @default.
• W1520171873 modified "2023-10-13" @default.
• W1520171873 title "Tectonic control on sedimentation, erosion and redeposition of Upper Jurassic sandstones, Central Graben, North Sea" @default.
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• W1520171873 cites W1984110690 @default.
• W1520171873 cites W1992390304 @default.
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• W1520171873 doi "https://doi.org/10.1002/9781118920435.ch17" @default.
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