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The Gulf of Mexico

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GEOSCIENCE EXPLAINED





The Gulf of Mexico Phase 3 Phase 2







Exploration interest in the deepwater US Gulf of Mexico is at an all time high with the deep water “Wilcox” sand Map showing extent of the Deep Focus seismic survey.

Deep Structure Phase 1 is shown in blue. Planned Phase 1

play being the main reservoir target. phases 2 and 3 areas shown in grey Bouguer gravity over Phase 1.



0.00 0.00 0.00 0.00

0.000





0.00-1000.00 -1000.000

-1000.00-100



Bjørnøya Basin Bjørnøyarenna Fault Cmplex Loppa High Hammerfest Basin

0.00-2000.00 -2000.000

-2000.00-200





0.00-3000.00 -3000.000

-3000.00-300

Top

Top Salt Salt

0.00-4000.00 -4000.000

-4000.00-400





0.00-5000.00

Salt

Base Base Salt -5000.000

-5000.00-500





0.00-6000.00 -6000.000

-6000.00-600





0.00-7000.00 -7000.000

-7000.00-700

Base Creataceous



0.00-8000.00 -8000.000

-8000.00-800





0.00-9000.00 -9000.00-900

-9000.000

Top Wilcox

Top Wilcox

-10000.00

0.00 -10000.00

-100

-10000.000



Mid Cretaceous Unconformity (MCU)

Mid Cretaceous Unconformity (MCU)

-11000.00

0.00 -11000.000

-110

-11000.00





-12000.00

0.00 -12000.000

-120

-12000.00





-13000.00

0.00 -13000.000

-130

-13000.00



Acoustic Basement

Acoustic Basement

-14000.00

0.00 Permian Carbonats -140

-14000.000

-14000.00





-15000.00

0.00 -15000.00

-150

-15000.000





-16000.00

0.00 -16000.000

-160

-16000.00





-17000.00 40

0.00 GEO ExPro Desember 2007 GEO ExPro Des ember 2007 -170

-17000.000

42 -17000.00

H o u s t o n , Texa s

GEOSCIENCE EXPLAINED TECHNOLOGY EXPLAINED

G e o r g e R . B r ow n C o n ve n t i o n C e n t e r



Deep Structure: Strength through

integration in the deepwater Gulf of Mexico

Exploration interest in the deepwater US Gulf of Mexico is at an all time high following the discovery, in

2001, of thick Paleogene submarine turbidites sand in the Baha #2 well. This ‘Wilcox’ sand play has now

Coming Soon

expanded across most of the deepwater and is the main reservoir target. These reservoir targets are typi-

cally 3 and 4 way structural closures, obscured by a thick allochthonous salt canopy and cored by deep

allochthonous salt.

Other potential deepwater plays include tionship underneath salt and enabled us

the Late Jurassic Norphlet aeolian dune to trace some of these anomalies back

play and the Upper Cretaceous submarine under salt where seismic imaging is more

fan play in the Western deepwater Gulf. of a challenge.

These potential plays combined with the The new interpreted magnetic basement

Wilcox play ensure that the deepwater sec- was constructed using standard depth-

tor will be an important exploration target to-basement techniques. This quantitative

for many years to come. This was further analysis of the magnetic data was primarily

reinforced by the record-breaking MMS carried out by means of Werner deconvo-

lease sales for the Western and Central Gulf lution, Euler deconvolution and Peters half

of Mexico in 2007 and it is clear that the slope methods. Gravity data was used to

industry is looking to the sub-salt Wilcox help resolve areas of discrepancy between

play and other potential sub-salt plays as the basement surfaces prior to finalizing

the future of exploration in the region. the integrated basement surface.

Understanding these play-fairway

opportunities requires a regional, structural Constraining basement

and stratigraphic context for the Paleo- This integrated basement, together with

gene Wilcox including sub-salt sediment top and base allochthonous salt horizons

distribution and a better understanding of from the Deep Focus work outlined above,

the tectonic framework of the basement.

Moreover, mapping the structure of the

were then used as the cornerstone for 2D

and 3D gravity and magnetics inversion

February 7 - 8, 2008

rifted basement will progress our under- Image of a 2D gravity and magnetic model using 2ModTM. and forward modeling work. Again this

standing of its impact on sedimentation, integration has lead to a much better con-

the distribution of autochthonous salt, and strained basement for assigning density

the location of the Continental-Oceanic each dataset can be interpreted in isolation and susceptibility values.

Boundary (COB). and used as a stand-alone product, integra- Fugro has also developed a workflow Prospects

Despite the huge volume of seismic data tion of these datasets has lead to a better to distinguish basement signal from auto- Producing Properties

(2D and 3D) acquired in the region, one understanding of the sub-salt section and chthonous and deep allochthonous salt U.S. Onshore & Offshore Plays

of the most fundamental challenges fac- has produced a robust and comprehensive signals during the 3D modeling process. International Opportunities

ing the industry is the problem of sub-salt interpretation. The new interpretation and All of this work has lead to a new under-

Capital Providers

imaging. Even with the latest processing modeling results provide a solid platform standing of the morphology and structure

Infinite Networking

technologies, seismic imaging of the sub- for future exploration and research in the of the basement and sub-salt stratigraphy

Expecting 1,500 Booths & 15,000 Attendees

salt stratigraphic section is problematic due sub-salt arena. in the area of Phase 1 that could not have

to the Allochthonous salt canopy. The new integrated basement interpre- been achieved from using seismic data



“Deep Structure”

tation relies heavily on the seismic data

outboard of salt where seismic imaging

alone. The implication of all of this is that as

we move into planned Phases 2 and 3, the Register online at: www.napeexpo.com

The purpose of “Deep Structure” is to is best. This area has been called the cali- lessons learned and the techniques devel-

combat the sub-salt imaging problem by bration area and is the best area to com- oped will allow Fugro to better cope with

using an integrated approach. By integrat- pare the magnetic basement and acoustic the inevitable complexities that will be C a l l N A P E h e a d q u a r t e r s a t 8 1 7 . 3 0 6 . 7 1 7 1 f o r m o r e i n f o r m a t i o n.

ing long-offset (10km) Deep Focus seismic basement without the influence of a salt encountered as we work through Garden

data, high resolution marine gravity data canopy. Banks, Green Canyon and East Breaks.

and high resolution airborne magnetics In the calibration area we have looked We have also have also learned about The 2008 NAPE Expo is presented by NAPE Expo LP, comprised of

data, Fugro has significantly increased its at the relationship between acoustic base- the power of integration and its impor-

understanding of the sub-salt geology of ment and magnetic basement anomalies. tance in geophysical and geological inter- AAPL, IPAA, SEG and AAPG as limited partners.

the Deepwater Gulf of Mexico. Although This allowed us to better assess the rela- pretation.





43 GEO ExPro Desember 2007 44 GEO ExPro Des ember 2007 GEO ExPro September 2007 47



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