taken from: alistair r. brown, aapg memoir 42, interpretation of three- dimensional seismic data,...

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Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three-Dimensional Seismic Data, 4th & 6th Editions John N. Louie, Presenter Tuning Phenomena in Reservoirs Effect of Tuning on Stratigraphic Interpretation Deterministic Tuning Curves Statistical Tuning Curves Understanding the Magnitude of Tuning Geol 755: Basin Analysis Geol 755: Basin Analysis Geophysics Week 6 Geophysics Week 6

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Page 1: Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three- Dimensional Seismic Data, 4th & 6th Editions John N. Louie, Presenter Tuning Phenomena

Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three-Dimensional Seismic Data, 4th & 6th Editions

John N. Louie, Presenter

Tuning Phenomena in ReservoirsEffect of Tuning on Stratigraphic Interpretation

Deterministic Tuning Curves

Statistical Tuning Curves

Understanding the Magnitude of Tuning Effects

John N. Louie, Presenter

Tuning Phenomena in ReservoirsEffect of Tuning on Stratigraphic Interpretation

Deterministic Tuning Curves

Statistical Tuning Curves

Understanding the Magnitude of Tuning Effects

Geol 755: Basin AnalysisGeol 755: Basin AnalysisGeophysics Week 6Geophysics Week 6

Geol 755: Basin AnalysisGeol 755: Basin AnalysisGeophysics Week 6Geophysics Week 6

Page 2: Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three- Dimensional Seismic Data, 4th & 6th Editions John N. Louie, Presenter Tuning Phenomena

Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three-Dimensional Seismic Data, 4th & 6th Editions

Effect of Tuning on Stratigraphic Interpretation When bed thickness ≥ When bed thickness ≥ , top and base reflections are separate., top and base reflections are separate. When bed thickness < When bed thickness < , reflections interfere and resonate- , reflections interfere and resonate- tuningtuning

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Page 3: Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three- Dimensional Seismic Data, 4th & 6th Editions John N. Louie, Presenter Tuning Phenomena

Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three-Dimensional Seismic Data, 4th & 6th Editions

Effect of Tuning on Stratigraphic Interpretation Where reflections merge, amplitude increasesWhere reflections merge, amplitude increases

Page 4: Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three- Dimensional Seismic Data, 4th & 6th Editions John N. Louie, Presenter Tuning Phenomena

Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three-Dimensional Seismic Data, 4th & 6th Editions

Effect of Tuning on Stratigraphic Interpretation In vertical and horizon section, amplitudes are highest where bed is thin- at In vertical and horizon section, amplitudes are highest where bed is thin- at

the the tuning thickness.the the tuning thickness. Merged downdip reflections average the dip of the reservoir top & base.Merged downdip reflections average the dip of the reservoir top & base.

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Page 5: Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three- Dimensional Seismic Data, 4th & 6th Editions John N. Louie, Presenter Tuning Phenomena

Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three-Dimensional Seismic Data, 4th & 6th Editions

Effect of Tuning on Stratigraphic Interpretation

The The limit of limit of visibilityvisibility depends on depends on thickness as thickness as well as well as impedance impedance contrast, and contrast, and noise levelnoise level

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Page 6: Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three- Dimensional Seismic Data, 4th & 6th Editions John N. Louie, Presenter Tuning Phenomena

Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three-Dimensional Seismic Data, 4th & 6th Editions

Deterministic Tuning Curves Have to Have to

differentiate differentiate tuning effects tuning effects from variations from variations in propertiesin properties (like porosity (like porosity and fluid and fluid content)content)

Tuning is a Tuning is a purelypurely geometricgeometric effect effect

The ideal tuning The ideal tuning thickness is thickness is /4/4

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Page 7: Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three- Dimensional Seismic Data, 4th & 6th Editions John N. Louie, Presenter Tuning Phenomena

Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three-Dimensional Seismic Data, 4th & 6th Editions

Deterministic Tuning Curves Sidelobes of wavelets also tune for thicker intervalsSidelobes of wavelets also tune for thicker intervals

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Page 8: Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three- Dimensional Seismic Data, 4th & 6th Editions John N. Louie, Presenter Tuning Phenomena

Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three-Dimensional Seismic Data, 4th & 6th Editions

Deterministic Tuning Curves

Different wavelets will Different wavelets will tune to different degreestune to different degrees

May be multiple maxima May be multiple maxima on the tuning curveon the tuning curve QuickTime™ and a

decompressorare needed to see this picture.

Page 9: Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three- Dimensional Seismic Data, 4th & 6th Editions John N. Louie, Presenter Tuning Phenomena

Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three-Dimensional Seismic Data, 4th & 6th Editions

Statistical Tuning Curves

Can Can cross-plotcross-plot amplitudes amplitudes from related from related locations to locations to examine examine correlationscorrelations

Linearity here Linearity here suggests suggests changes changes withinwithin reservoir, not reservoir, not outsideoutside

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Page 10: Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three- Dimensional Seismic Data, 4th & 6th Editions John N. Louie, Presenter Tuning Phenomena

Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three-Dimensional Seismic Data, 4th & 6th Editions

Statistical Tuning Curves

Reflection Reflection amplitude amplitude against against interpreted interpreted thicknessthickness

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Page 11: Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three- Dimensional Seismic Data, 4th & 6th Editions John N. Louie, Presenter Tuning Phenomena

Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three-Dimensional Seismic Data, 4th & 6th Editions

Statistical Tuning Curves

Reflection Reflection amplitude amplitude against against interpreted interpreted thicknessthickness

The The envelopeenvelope is is a statistical a statistical tuning curvetuning curve

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Page 12: Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three- Dimensional Seismic Data, 4th & 6th Editions John N. Louie, Presenter Tuning Phenomena

Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three-Dimensional Seismic Data, 4th & 6th Editions

Statistical Tuning Curves

Reflection Reflection amplitude amplitude against against interpreted interpreted thicknessthickness

The The envelopeenvelope here follows here follows a percentile a percentile of of amplitudesamplitudes

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Page 13: Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three- Dimensional Seismic Data, 4th & 6th Editions John N. Louie, Presenter Tuning Phenomena

Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three-Dimensional Seismic Data, 4th & 6th Editions

Statistical Tuning Curves

Reflection Reflection amplitude amplitude against against interpreted interpreted thicknessthickness

The The envelopeenvelope here is here is compared compared with a deter-with a deter-ministic ministic curvecurve

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Page 14: Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three- Dimensional Seismic Data, 4th & 6th Editions John N. Louie, Presenter Tuning Phenomena

Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three-Dimensional Seismic Data, 4th & 6th Editions

Understanding the Magnitude of Tuning Effects Wavelet shape is critical to knowing where tuning is occurring.Wavelet shape is critical to knowing where tuning is occurring.

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Page 15: Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three- Dimensional Seismic Data, 4th & 6th Editions John N. Louie, Presenter Tuning Phenomena

Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three-Dimensional Seismic Data, 4th & 6th Editions

Understanding the Magnitude of Tuning Effects Wavelet shape is critical to knowing where tuning is occurring.Wavelet shape is critical to knowing where tuning is occurring.

QuickTime™ and a decompressor

are needed to see this picture.

Page 16: Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three- Dimensional Seismic Data, 4th & 6th Editions John N. Louie, Presenter Tuning Phenomena

Taken From: Alistair R. Brown, AAPG Memoir 42, Interpretation of Three-Dimensional Seismic Data, 4th & 6th Editions

Understanding the Magnitudeof Tuning Effects

““The first side lobe as a fraction of the center lobe of a The first side lobe as a fraction of the center lobe of a zero-phase wavelet is the reciprocal of the octave zero-phase wavelet is the reciprocal of the octave bandwidthbandwidth.”.”

Good seismic data has 2.5 octaves, for a side lobe level of Good seismic data has 2.5 octaves, for a side lobe level of 40% relative to the center.40% relative to the center.

This “40% rule” means that 40% is a common increase in This “40% rule” means that 40% is a common increase in amplitude at tuning for zero phase wavelets, reflected from amplitude at tuning for zero phase wavelets, reflected from the top and base of a reservoir layer.the top and base of a reservoir layer.

Greater increases in amplitude must be explained Greater increases in amplitude must be explained otherwise.otherwise.