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Seismic geomorphological analysis and hydrocarbon potential of the Lower Cretaceous Cromer Seismic geomorphological analysis and hydrocarbon potential of the Lower Cretaceous Cromer

Seismic geomorphological analysis and hydrocarbon potential of the Lower Cretaceous Cromer - PowerPoint Presentation

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Seismic geomorphological analysis and hydrocarbon potential of the Lower Cretaceous Cromer - PPT Presentation

Heidrun field Norway Paper by Moscardelli and Wood Main objective One of the main objectives of this study is to characterize the architecture and geomorphology of the Cromer Knoll Group within the ID: 927918

group cretaceous heidrun field cretaceous group field heidrun cromer knoll reservoirs jurassic potential seismic oil upper unconformities norwegian terrace

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Presentation Transcript

Slide1

Seismic geomorphological analysis and hydrocarbon potential of the Lower Cretaceous Cromer Knoll Group, Heidrun field, Norway

Paper by:

Moscardelli

and Wood

Slide2

Slide3

Main objective:“One of the main objectives of this study is to characterize the architecture and geomorphology of the Cromer Knoll Group within the Heidrun Field to explain the tectonostratigraphic significance, paleoenviromental

configuration, and reservoirs potential of this Lower Cretaceous

postrift

unit.” –

Moscardelli

and Wood

Slide4

Halten Terrace was one of the first giant oil fields found in Norwegian Sea.Narrow continental shelf due to faulting.Has been producing from Jurassic reservoirs the last 30years.Heidrun field in 1985 had 750 million

bbl

of recoverable oil.

Things to note:

Slide5

Wanted to focus on Upper Cretaceous units in the Heidrun Field.Contains thick shales that act as seals from Upper Jurassic reservoirs.

Cromer Knoll Group

Slide6

Used 3D seismic reflection data and well data to examine Lower Cretaceous wedge.Cromer Knoll Group is within the hanging wall of a half graben in the Halten Terrace.This half

graben

has potential of high quality Cretaceous sandstones.

What they did:

Slide7

Slide8

Basement of mid-Norwegian basin is Caledonian metamorphic and intrusive rocks.Basin is affected by rifting and faults.Accumulation of thousands of meters of sediment.Ten unconformities have been interpreted.

Unconformities bounded six

tectonosequences

.

History of

Heidrun

Field

Slide9

Slide10

Slide11

T1 formed structural traps and migration paths for hydrocarbon accumulations.T3 (Shetland Group) act as potential seals for Lower Cretaceous intervals.Spekk Formation is the primary oil and gas source rock.A fault connects T1 (Triassic and Jurassic) and T2 (Lower Cretaceous) and suggests that upward fluid migration might be possible.

What they found:

Slide12

Although the Jurassic reservoirs are reaching their limit, there is a high possibility that hydrocarbons are in the upper part of the Cromer Knoll Group of the Heidrun Field off the shore of Norway, according to the lithological and seismic analysis.In conclusion….