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Jamie Rich Kurt Marfurt University of Oklahoma ConocoPhillips School of Geology and Geophysics.

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Presentation on theme: "Jamie Rich Kurt Marfurt University of Oklahoma ConocoPhillips School of Geology and Geophysics."— Presentation transcript:

1 Jamie Rich Kurt Marfurt University of Oklahoma ConocoPhillips School of Geology and Geophysics

2  Curvature is commonly used along side coherency to characterize faulting  Curvature quantifies the degree of bending on a surface and is generalized as a volumetric attribute  We must consider direction and magnitude of curvature

3 Direction of curvature measurement Circle with a radius equal to the inverse of curvature Largest curvature Smallest curvature

4 Direction of curvature measurement Circle with a radius equal to the inverse of curvature Largest curvature Smallest curvature

5 Direction of curvature measurement Circle with a radius equal to the inverse of curvature Largest curvature Smallest curvature

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7 White, 2013 Largest Magnitude Negative Curvature Largest Magnitude Positive Curvature

8 Mai, 2010

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13  In order to better locate the fault we are interested in the inflection point  Where does the curvature change sign?  Is that change positive or negative?  Coherency can’t tell us this!

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15 Gao, 2013

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21 Xline N Inline

22 Xline N

23 Gao, 2013

24 Xline N Inline

25 Xline N

26 N Inline

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28  Differentials of curvature (Flexure) can be useful for defining fault planes  Care must be used when defining directions and signs  Further consideration and 3D application may expand usefulness


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