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UK Cont<strong>in</strong>ental Shelf:<br />

Rais<strong>in</strong>g <strong>the</strong> Bar for Regional 3D<br />

Seismic <strong>in</strong> <strong>the</strong> Central North Sea<br />

Depth <strong>in</strong><br />

metres<br />

0 –<br />

1,000 –<br />

North-West<br />

Random l<strong>in</strong>e oriented north-west to south-east across <strong>the</strong> data, <strong>in</strong>tersect<strong>in</strong>g several fields (modified from<br />

Holl<strong>in</strong>gworth et al., 2015). The f<strong>in</strong>al velocity model is co-rendered with <strong>the</strong> PSDM full-stack amplitude data<br />

highlight<strong>in</strong>g both geologically consistent regional trends along with local facies variations.<br />

Shelley<br />

North South<br />

High-quality and well-positioned seismic data are key requirements of <strong>the</strong> decision-mak<strong>in</strong>g<br />

process to recover <strong>the</strong> rema<strong>in</strong><strong>in</strong>g and bypassed hydrocarbons <strong>in</strong> mature areas. A great<br />

deal of seismic exploration has taken place with<strong>in</strong> <strong>the</strong> Central North Sea, us<strong>in</strong>g a variety<br />

of acquisition configurations <strong>in</strong>clud<strong>in</strong>g <strong>the</strong> latest broadband solutions. Through decades<br />

of exploration, most surveys <strong>in</strong> this mature bas<strong>in</strong> have been reprocessed multiple times as<br />

techniques have evolved and, every so often, significant advances <strong>in</strong> technology warrant<br />

<strong>the</strong> application of <strong>the</strong>se new approaches <strong>in</strong> a wholesale way. This is what CGG has recently<br />

achieved with new seismic acquisition and reprocess<strong>in</strong>g of key multi-client surveys cover<strong>in</strong>g<br />

<strong>the</strong> entire Central Graben <strong>in</strong> <strong>the</strong> North Sea.<br />

Andrew Montrose Madoes Fram Acorn<br />

Top Paleocene<br />

horizon<br />

High-velocity Cretaceous chalk<br />

with rapid lateral variations<br />

Detached<br />

salt diapir<br />

South-East<br />

Velocity<br />

<strong>in</strong> m/s<br />

– 1,480<br />

– 1,600<br />

– 1,900<br />

– 2,200<br />

2,000 –<br />

– 2,500<br />

– 2,800<br />

3,000 –<br />

– 3,100<br />

– 3,400<br />

4,000 –<br />

– 3,700<br />

– 4,000<br />

5,000 –<br />

Mid North-Sea High<br />

– 4,300<br />

– 4,600<br />

6,000 –<br />

– 4,900<br />

– 5,200<br />

7,000 –<br />

Base Cretaceous<br />

Unconformity<br />

Montrose High<br />

Rotated Triassic pods between<br />

higher-velocity salt walls<br />

– 5,500<br />

– 5,800<br />

– 5,980<br />

8,000 –<br />

64 GEOExPro November 2015 GEOExPro November 2015 66

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