int e-p1: attribute applications @ seg 2017 3d curvature...

17
3D curvature analysis of seismic waveform & its interpretational implications Haibin Di, Motaz Alfarraj, and Ghassan AlRegib Center for Energy & Geo Processing (CeGP) Georgia Institute of Technology {hdi7, motaz, alregib}@ece.gatech.edu September 25, 2017 INT E-P1: Attribute Applications @ SEG 2017

Upload: others

Post on 19-Jul-2020

5 views

Category:

Documents


0 download

TRANSCRIPT

Page 1: INT E-P1: Attribute Applications @ SEG 2017 3D curvature ...ghassanalregibdotcom.files.wordpress.com/2016/10/haibin_seg2017_3d.pdfWaveform Curvature: 2D section 6 Take inline section

3D curvature analysis of seismic waveform & its interpretational

implicationsHaibin Di, Motaz Alfarraj, and Ghassan AlRegib

Center for Energy & Geo Processing (CeGP)Georgia Institute of Technology

{hdi7, motaz, alregib}@ece.gatech.eduSeptember 25, 2017

INT E-P1: Attribute Applications @ SEG 2017

Page 2: INT E-P1: Attribute Applications @ SEG 2017 3D curvature ...ghassanalregibdotcom.files.wordpress.com/2016/10/haibin_seg2017_3d.pdfWaveform Curvature: 2D section 6 Take inline section

Outline• Motivation• Waveform curvature vs. geometric curvature• Three implications• Application to horizon modeling• Conclusions

2

Page 3: INT E-P1: Attribute Applications @ SEG 2017 3D curvature ...ghassanalregibdotcom.files.wordpress.com/2016/10/haibin_seg2017_3d.pdfWaveform Curvature: 2D section 6 Take inline section

Motivation• Curvature analysis is useful for measuring the reflector geometry to

depict the surface morphology and highlight the potential faults and fractures caused by anticlinal bending (e.g., Roberts, 2001);

• The reflector geometry is only partial information offered in a seismic cube, and the reflection waveform is also of significant importance for interpreting the seismic signals;

• What if applying the curvature analysis to the reflection waveforms?

3

Page 4: INT E-P1: Attribute Applications @ SEG 2017 3D curvature ...ghassanalregibdotcom.files.wordpress.com/2016/10/haibin_seg2017_3d.pdfWaveform Curvature: 2D section 6 Take inline section

Curvature

4

𝑘𝑘2𝐷𝐷(x, z) =𝑧𝑧′′

1 + 𝑧𝑧′2⁄3 2

𝑘𝑘3𝐷𝐷𝑚𝑚𝑚𝑚𝑚𝑚 𝑥𝑥,𝑦𝑦, 𝑧𝑧 = MAX(𝑘𝑘3𝐷𝐷𝜑𝜑 𝑥𝑥,𝑦𝑦, 𝑧𝑧 , 𝜑𝜑=[0o, 360o))

𝑘𝑘3𝐷𝐷𝑚𝑚𝑖𝑖𝑖𝑖 𝑥𝑥,𝑦𝑦, 𝑧𝑧 = MIN(𝑘𝑘3𝐷𝐷𝜑𝜑 𝑥𝑥,𝑦𝑦, 𝑧𝑧 , 𝜑𝜑=[0o, 360o))

where 𝑘𝑘3𝐷𝐷𝜑𝜑 𝑥𝑥, 𝑦𝑦, 𝑧𝑧 = 1

1+𝐴𝐴12+𝐴𝐴22⁄1 2 �

𝐵𝐵1+𝐵𝐵2 tan2 𝜑𝜑+2𝐵𝐵3𝑡𝑡𝑚𝑚𝑖𝑖𝜑𝜑1+𝐴𝐴12 + 1+𝐴𝐴22 𝑡𝑡𝑚𝑚𝑖𝑖2𝜑𝜑+2𝐴𝐴1𝐴𝐴2𝑡𝑡𝑚𝑚𝑖𝑖𝜑𝜑

Page 5: INT E-P1: Attribute Applications @ SEG 2017 3D curvature ...ghassanalregibdotcom.files.wordpress.com/2016/10/haibin_seg2017_3d.pdfWaveform Curvature: 2D section 6 Take inline section

Waveform Curvature: 1D trace

5

𝑘𝑘2𝐷𝐷(z, w) =𝑤𝑤′′

1 + 𝑤𝑤′2 ⁄3 2

where z: vertical coordinatew: waveform amplitude

2nd-order derivative resolution enhancement

Page 6: INT E-P1: Attribute Applications @ SEG 2017 3D curvature ...ghassanalregibdotcom.files.wordpress.com/2016/10/haibin_seg2017_3d.pdfWaveform Curvature: 2D section 6 Take inline section

Waveform Curvature: 2D section

6

Take inline section for example:

𝒌𝒌𝟑𝟑𝟑𝟑𝒎𝒎𝒎𝒎𝒎𝒎 𝒎𝒎, 𝒛𝒛,𝒘𝒘 = MAX(𝒌𝒌𝟑𝟑𝟑𝟑𝝋𝝋 𝒎𝒎, 𝒛𝒛,𝒘𝒘 , 𝝋𝝋=[0o, 360o)) (in blue)

𝒌𝒌𝟑𝟑𝟑𝟑𝒎𝒎𝒎𝒎𝒎𝒎 𝒎𝒎, 𝒛𝒛,𝒘𝒘 = MIN(𝒌𝒌𝟑𝟑𝟑𝟑𝝋𝝋 𝒎𝒎, 𝒛𝒛,𝒘𝒘 , 𝝋𝝋=[0o, 360o)) (in red)

where x: crossline coordinatez: vertical coordinatew: waveform amplitude

Crossline No.

SampleNo.

Page 7: INT E-P1: Attribute Applications @ SEG 2017 3D curvature ...ghassanalregibdotcom.files.wordpress.com/2016/10/haibin_seg2017_3d.pdfWaveform Curvature: 2D section 6 Take inline section

Waveform Curvature

7

Geometric curvature Waveform curvatureObject Curvature analysis of seismic signals

Information for analysis

a. Structural depth/timeb. Reflection amplitude Reflection waveform

Computation direction

Horizontal(the 𝑥𝑥-𝑦𝑦 plane)

Vertical(the 𝑥𝑥-𝑧𝑧 and/or 𝑦𝑦-𝑧𝑧 plane)

Implications

Structure analysis:a. Fault detectionb. Fracture characterizationc. Reflector morphology

delineation

Waveform analysis:a. Resolution enhancementb. Dip estimation c. Reflector decomposition

Table: Geometric curvature vs. waveform curvature

Page 8: INT E-P1: Attribute Applications @ SEG 2017 3D curvature ...ghassanalregibdotcom.files.wordpress.com/2016/10/haibin_seg2017_3d.pdfWaveform Curvature: 2D section 6 Take inline section

Implication #1: Resolution enhancement

8Original amplitude section Maximum waveform curvature

a. Curvature: 2nd-order derivative better resolutionb. Maximum curvature: Normal to the reflection more reliable analysis

Page 9: INT E-P1: Attribute Applications @ SEG 2017 3D curvature ...ghassanalregibdotcom.files.wordpress.com/2016/10/haibin_seg2017_3d.pdfWaveform Curvature: 2D section 6 Take inline section

Implication #2: Dip estimation

9

Minimum curvature: Parallel to the reflection reflector dip

Orientation of Minimum waveform curvature Dip-guided horizon tracking

More in my next presentation at 3:05 pm

Page 10: INT E-P1: Attribute Applications @ SEG 2017 3D curvature ...ghassanalregibdotcom.files.wordpress.com/2016/10/haibin_seg2017_3d.pdfWaveform Curvature: 2D section 6 Take inline section

Implication #3: Reflector decomposition

10

Peaks Troughs

S-crossings Z-crossings

Page 11: INT E-P1: Attribute Applications @ SEG 2017 3D curvature ...ghassanalregibdotcom.files.wordpress.com/2016/10/haibin_seg2017_3d.pdfWaveform Curvature: 2D section 6 Take inline section

Application to horizon modeling

11

Peak decomposition Thinning

Seed picking and sortingSeeded horizon trackingHorizon model

Seismic image

Page 12: INT E-P1: Attribute Applications @ SEG 2017 3D curvature ...ghassanalregibdotcom.files.wordpress.com/2016/10/haibin_seg2017_3d.pdfWaveform Curvature: 2D section 6 Take inline section

Limitations• Sensitivity to high-frequency components• Sensitivity to vertical window size• Sensitivity to seismic noises

12

Page 13: INT E-P1: Attribute Applications @ SEG 2017 3D curvature ...ghassanalregibdotcom.files.wordpress.com/2016/10/haibin_seg2017_3d.pdfWaveform Curvature: 2D section 6 Take inline section

Limitation #1: Sensitivity to high-frequency components

13

Maximum waveform curvature

Original amplitude

-15000 +15000

-0.5 +0.5

Take Ricker wavelet for example𝑤𝑤 𝑡𝑡 = 𝐴𝐴 � 1 − 2𝜋𝜋2𝑓𝑓𝑀𝑀

2𝑡𝑡2 𝑒𝑒−𝜋𝜋2𝑓𝑓𝑀𝑀2𝑡𝑡2

Waveform curvature:𝑘𝑘 0,𝑤𝑤 = 6 � 𝐴𝐴 � 𝜋𝜋2𝑓𝑓𝑀𝑀

2

• Linear to amplitude A• quadratic to frequency f

Page 14: INT E-P1: Attribute Applications @ SEG 2017 3D curvature ...ghassanalregibdotcom.files.wordpress.com/2016/10/haibin_seg2017_3d.pdfWaveform Curvature: 2D section 6 Take inline section

Limitation #2: Sensitivity to vertical window size

14

Z

Window size = 7

Window size = 3

Window size = 9

Window size = 5

-0.5 +0.5

Window size no larger than half of the waveform period

Page 15: INT E-P1: Attribute Applications @ SEG 2017 3D curvature ...ghassanalregibdotcom.files.wordpress.com/2016/10/haibin_seg2017_3d.pdfWaveform Curvature: 2D section 6 Take inline section

Limitation #3: Sensitivity to seismic noise

15-0.5 +0.5

From smoothed seismic

From original seismic

For resolution enhancement: use original amplitude

For dip estimation :Apply smoothing first

For horizon interpretation:Apply smoothing first

Page 16: INT E-P1: Attribute Applications @ SEG 2017 3D curvature ...ghassanalregibdotcom.files.wordpress.com/2016/10/haibin_seg2017_3d.pdfWaveform Curvature: 2D section 6 Take inline section

Conclusions• Curvature analysis is extended to seismic waveforms;• Several implications:

• Resolution enhancement along the direction normal to seismic reflectors• Dip estimation• Reflector decomposition to peaks, troughs, and z/s-crossings;

• Potentials for horizon interpretation and modelling

16

Page 17: INT E-P1: Attribute Applications @ SEG 2017 3D curvature ...ghassanalregibdotcom.files.wordpress.com/2016/10/haibin_seg2017_3d.pdfWaveform Curvature: 2D section 6 Take inline section

17

More information (e.g., recent research, publications, tools, and codes) is available by:Visit our booth: #2109Visit our center: http://www.ghassanalregib.comVisit my webpage: https://sites.google.com/site/dihaibin/