2011Marine Geology FrontiersRequires access

TECTONIC-SEDIMENTARY EVOLUTION OF JURASSIC IN VIKING GRABEN,THE NORTH SEA

Yang Chuansheng

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Abstract

The Jurassic contains the major source rock in the Viking Graben,with shallow-marine sandstones and deep-water submarine-fan sandstones as main reservoirs.Careful study of tectonic-sedimentary evolution is the key to oil and gas exploration.The Jurassic in the Viking Graben could be divided to two phases: Early-Middle Jurassic thermal subsidence and Late Jurassic active stretching phases.In the early stage of the thermal subsidence phase,marine depositional environments prevailed.But in the Middle Jurassic stage it is dominated by a non-marine delta depositional system.In the phase of active stretching,there formed a deep-water submarine-fan system.Based on the facts mentioned above,two tectonic-sedimentary models were established for the Jurassic in Viking Graben of the North Sea.

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The Jurassic contains the major source rock in the Viking Graben,with shallow-marine sandstones and deep-water submarine-fan sandstones as main reservoirs.Careful study of tectonic-sedimentary evolution is the key to oil and gas exploration.The Jurassic in the Viking Graben could be divided to two phases: Early-Middle Jurassic thermal subsidence and Late Jurassic active stretching phases.In the early stage of the thermal subsidence phase,marine depositional environments prevailed.But in the Middle Jurassic stage it is dominated by a non-marine delta depositional system.In the phase of active stretching,there formed a deep-water submarine-fan system.Based on the facts mentioned above,two tectonic-sedimentary models were established for the Jurassic in Viking Graben of the North Sea.

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Available abstract

The Jurassic contains the major source rock in the Viking Graben,with shallow-marine sandstones and deep-water submarine-fan sandstones as main reservoirs.Careful study of tectonic-sedimentary evolution is the key to oil and gas exploration.The Jurassic in the Viking Graben could be divided to two phases: Early-Middle Jurassic thermal subsidence and Late Jurassic active stretching phases.In the early stage of the thermal subsidence phase,marine depositional environments prevailed.But in the Middle Jurassic stage it is dominated by a non-marine delta depositional system.In the phase of active stretching,there formed a deep-water submarine-fan system.Based on the facts mentioned above,two tectonic-sedimentary models were established for the Jurassic in Viking Graben of the North Sea.

Key concepts: Geology, Graben, Sedimentary depositional environment, Sedimentary rock, Paleontology, Tectonic subsidence, Subsidence, Tectonics

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