Structural geology Faults and the implications on fluid flow 1 - Classification: Internal 2011-02-10 • Intro – What is structural geology? – Structural geological data • Structural geology on Gullfaks – Regional and field scale • Faults and how they affect the fluid flow in Gullfaks H1 segment 2 - Classification: Internal 2011-02-10 STRUCTURAL GEOLOGY Treats (deformation-) structures in the earths crust and how they are formed. For Gullfaks these structures are mainly faults 3 - Classification: Internal 2011-02-10 FAULTS A surface, or more commonly, a narrow zone along which one of the sides has been displace past the other side. Normal 4 - Classification: Internal 2011-02-10 Revers Sidelengs Databasis for structural interpretation • Seismic data – Structural processed cubes – Offset-cubes – 4D seismic • Data from more than 200 wells – Cores (more than 8 km) – Detailed logs – Production data – Pressure data • Field analogs (Utah) 5 - Classification: Internal 2011-02-10 200 m 500 m No info regarding: Sub-seismic faults Fault zone Fault seal 6 - Classification: Internal 2011-02-10 Field analogs (Utah) 7 - Classification: Internal 2011-02-10 Structural geology on Gullfaks – regional scale 8 - Classification: Internal 2011-02-10 9 - Classification: Internal 2011-02-10 Structural development on Gullfaks - keywords • Two regional rifting periods: – (Perm)-Triassic – Middle Jurassic – Early Cretaceous • Internally on Gullfaks mainly as a result of late Jurassic-early Cretaceous deformation – Regional thickness variations on the Brent-Group indicates fault development started in middle Jurassic • Core studies show that Brent was poorly consolidated (not deep buried) at the time of deformation – This has implications on what kind of structures develop • Brent (middle Jurassic) was deposited in pre-tectonic time 10 - Classification: Internal 2011-02-10 Structural geology in the Tampen area 11 - Classification: Internal 2011-02-10 Structural geology on Gullfaks – field scale 12 - Classification: Internal 2011-02-10 Strukturgeologi Domino system • Faults: 20-30º dip towards east • Fault geometry is more complex in Brent than Statfjord • Layering: ca. 15 degrees towards west • Internal deformation Accomodation • Mest complex area on Gullfaks regarding sctructures Cook (Dunlin) Horst complex • Faults: 60-70º dip towards west • Sub-horisontal layering • Less internal deformation 13 - Classification: Internal 2011-02-10 Gullfaks South 14 - Classification: Internal 2011-02-10 Data collection at different scales Variation of resolution 15 - Classification: Internal 2011-02-10 Coredata (9 m throw) 34/10-A-15 34/10-B-12 16 - Classification: Internal 2011-02-10 Faults and the implication on fluid flow 17 - Classification: Internal 2011-02-10 18 - Classification: Internal 2011-02-10 Juxtaposition without seal Juxtaposition with seal (clay smear) 19 - Classification: Internal 2011-02-10 Models/seismic interpretaion 20 - Classification: Internal 2011-02-10 Real? Thank you Presentation title Presenters name Presenters title E-mail address, tel: +00 00 00 00 www.statoil.com 21 - Classification: Internal 2011-02-10