Depth and dip calculations using velocity functions
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| Series | Geophysical References Series |
|---|---|
| Title | Problems in Exploration Seismology and their Solutions |
| Author | Lloyd P. Geldart and Robert E. Sheriff |
| Chapter | 4 |
| Pages | 79 - 140 |
| DOI | http://dx.doi.org/10.1190/1.9781560801733 |
| ISBN | ISBN 9781560801153 |
| Store | SEG Online Store |
Problem 4.15a
Repeat the calculations of problem 4.14 assuming horizontal velocity layering and dip moveout of 104 ms/km, and find the dips.
Background
While velocity generally follows the layering, especially in structurally deformed areas, isovelocity surfaces may not parallel interfaces. Where the section has not been uplifted significantly, isovelocity surfaces are apt to be nearly horizontal in spite of structural relief.
Solution
The depths will be the same as those calculated in problem 4.14 except that $ z $ is now slant depth. Vertical depths are $ z_{v}=z\cos \xi $, where the dip $ \xi $ is given by $ \sin ^{-1}(V\Delta t_{d}/2\Delta x)=\sin ^{-1}(0.052\ V) $, $ V $ usually being either $ {\bar {V}} $ or $ V_{\rm {rms}} $. Using the values of $ t_{0} $, $ {\bar {V}} $ and Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): V_{\rm rms} from Table 4.14a, we obtain the results in Table 4.15a.
| Time | Velocity | Slant | Dip | Vert. depth |
|---|---|---|---|---|
| Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): t_0 | Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): V | depth | Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): \xi | Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): z \cos \xi |
| i) Assuming average velocities: | ||||
| 1.00 s | 2.00 km/s | 1000 m | 5.97Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): ^{\circ} | 990 m |
| 2.00 | 2.50 | 2500 | 7.47 | 2480 |
| 2.10 | 2.67 | 2800 | 7.98 | 2770 |
| 3.10 | 3.10 | 4800 | 9.28 | 4740 |
| ii) Assuming rms velocities: | ||||
| 1.00 s | 2.99 km/s | 1000 m | 5.97$ ^{\circ } $ | 990 m |
| 2.00 | 2.55 | 2550 | 7.62 | 2530 |
| 2.10 | 2.81 | 2950 | 8.40 | 2920 |
| 3.10 | 3.24 | 5020 | 9.70 | 4950 |
| iii) Assuming best-fit depth function: | ||||
| 1.00 s | 2.02 km/s | 1010 m | 6.03Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): ^{\circ} | 1000 m |
| 2.00 | 2.54 | 2540 | 7.59 | 2520 |
| 2.10 | 2.59 | 2720 | 7.74 | 2700 |
| 3.10 | 3.12 | 4840 | 9.34 | 4780 |
| iv) Assuming best-fit traveltime function: | ||||
| 1.00 s | 2.03 km/s | 1020 m | 6.00Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): ^{\circ} | 1010 m |
| 2.00 | 2.62 | 2620 | 7.83 | 2800 |
| 2.10 | 2.68 | 2810 | 8.01 | 2780 |
| 3.10 | 3.27 | 5270 | 9.79 | 5000 |
Problem 4.15b
Trace rays assuming (i) the velocity layering given in Figure 4.13a, and (ii) that the velocity is constant at the values of Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): \bar{V} and Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): V_{\rm rms} listed in Figure 4.13b. Find the arrival times and reflecting points of reflections at each of the interfaces.
Solution
i) We first calculate the angle of approach Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): \alpha [using equation (4.2d)] and then use Snell’s law to find the other angles:
Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): \begin{align} \alpha = \theta_1 &= \sin^{-1}\left(2.00\times \frac{0.104}{2}\right) = 6.0^{\circ}, \\ \sin\theta_2 &= (V_2/V_1)\sin \theta_1, \\ \theta_2 &= \sin^{-1}[(3.00/2.00) \sin 6.0^{\circ}] = 9.0^{\circ},\\ \theta_3 &= \sin^{-1}[(6.00/2.00) \sin 6.0^{\circ}] = 18.3^{\circ},\\ \theta_4 &= \sin^{-1}[(4.00/2.00) \sin 6.0^{\circ}] = 12.1^{\circ},\\ t_A &= 2z/(V_1 \cos \theta_1) = 2.000/(2.00 \cos 6.0^{\circ}) \\ &= 1.006\ \mathrm{s}, \\ t_B &= 1.006 + 2 \times 1.500/3.00 \cos 9.0^{\circ} \\ &= 2.018\ \mathrm{s}, \\ t_C &= 2.018 + 2 \times 0.300/6.00 \cos 18.3^{\circ} \\ &= 2.123\ \mathrm{s}, \\ t_D &= 2.123 + 2 \times 2.000/4.00 \cos 12.1^{\circ} \\ &= 3.146\ \mathrm{s}. \end{align}
Next we find $ x $-coordinates of intersections of rays and interfaces:
Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): \begin{align} x_A &= z\sin 6.0^{\circ} = 0.105\ \mathrm{km}, \\ x_B &= 0.105 + 0.156 = 0.261\ \mathrm{km}, \\ x_C &= 0.261 + 0.031 = 0.292\ \mathrm{km}, \\ x_D &= 0.292 + 0.209 = 0.501\ \mathrm{km}. \end{align}

ii) Assuming Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): \bar{V} = 0.288 z + 1.77 (see Figure 4.13b) and the given depths,
Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): \begin{align} V_A = 0.288 + 1.77 = 2.058\ \mathrm{km/s},\ \alpha = 6.1^{\circ}, \\ t_A = 2z/(V_1\cos\theta_1) = 0.977\ \mathrm{s}, \\ x_A = 2z \sin 6.1^{\circ} = 0.107\ \mathrm{km}; \\ V_B = 0.72 + 1.77 = 2.49\ \mathrm{km/s}, \alpha = 7.4^{\circ}, \\ t_B = 5.00/2.562\cos 7.4^{\circ} = 1.968\ \mathrm{s}, x_B = 0.324\ \mathrm{km}; \\ V_C = 0.806 + 1.77 = 2.576\ \mathrm{km/s}, \alpha = 7.7^{\circ}, \\ t_C = 5.600/2.660 \cos 7.7^\circ = 2.124\ \mathrm{s}, x_C = 0.365\ \mathrm{km}; \\ V_D = 1.382 + 1.77 = 2.940\ \mathrm{km/s}, \alpha = 9.4^{\circ} \\ t_D = 9.600/3.310\cos 9.4^{\circ} = 3.146\ \mathrm{s}, x_D = 0.787\ \mathrm{km}. \end{align}
Assuming Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): V_{\rm rms} = 0.325 z + 1.75 and the given depths,
Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): \begin{align} V_A = 0.325 + 1.75 = 2.075\ \mathrm{km/s}, \alpha = 6.2^\circ \\ t_A = 2z(V_1\cos\theta_1) = 2.00/(2.075\cos 6.2^\circ) = 0.970\ \mathrm{s} \\ x_A = 2z\sin 6.2^\circ = 0.108\ \mathrm{km}; \\ V_B = 0.812 + 1.75 = 2.562\ \mathrm{km/s}, \alpha = 7.7^\circ \\ t_B = 5.000/2.562\cos 7.7^\circ = 2.018\ \mathrm{s}, x_B = 0.335\ \mathrm{km}; \\ V_C = 0.910 + 1.75 = 2.660\ \mathrm{km/s}, \alpha = 8.0^\circ, \\ t_C = 5.600/2.660\cos 8.0^\circ = 2.123\ \mathrm{s}, x_C = 0.390\ \mathrm{km}; \\ V_D = 1.560 + 1.75 = 3.310\ \mathrm{km/s}, \alpha = 9.9^\circ, \\ t_D = 9.600/3.310\cos 9.9^\circ = 3.146\ \mathrm{s}, x_D = 0.825\ \mathrm{km}. \end{align}
Assuming Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): \bar{V} = 0.526t + 1.49 and times in part (i):
Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): \begin{align} t_A = 1.006\ \mathrm{s}, \bar{V} = 2.019\ \mathrm{km/s}, \alpha = 6.0^\circ, z_A = 2.042\ \mathrm{km}, x_A = 0.213\ \mathrm{km}, \\ t_B = 2.018\ \mathrm{s}, \bar{V} = 2.551\ \mathrm{km/s}, \alpha = 7.6^\circ, z_B = 5.194\ \mathrm{km}, x_B = 0.683\ \mathrm{km}, \\ t_C = 2.123\ \mathrm{s}, \bar{V} = 2.607\ \mathrm{km/s}, \alpha = 7.8^\circ, z_C = 5.586\ \mathrm{km}, x_C = 0.751\ \mathrm{km}, \\ t_D = 3.146\ \mathrm{s}, \bar{V} = 3.145\ \mathrm{km/s}, \alpha = 9.6^\circ, z_D = 10.029\ \mathrm{km}, x_D = 1.618\ \mathrm{km}. \end{align}
Assuming Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): V_{\rm rms} = 0.595\mathrm{t} + 1.43 and times in part (i):
Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): \begin{align} t_A = 1.006\ \mathrm{s}, V_{\rm rms} = 2.029\ \mathrm{km/s}, \alpha = 6.1^\circ, z_A = 2.053\ \mathrm{km}, x_A = 0.215\ \mathrm{km},\\ t_B = 2.018\ \mathrm{s}, V_{\rm rms} = 2.631\ \mathrm{km/s}, \alpha = 7.9^\circ, z_B = 5.360\ \mathrm{km}, x_B = 0.726\ \mathrm{km},\\ t_C = 2.123\ \mathrm{s}, V_{\rm rms} = 2.693\ \mathrm{km/s}, \alpha = 8.1^\circ, z_C = 5.774\ \mathrm{km}, x_C = 0.800\ \mathrm{km},\\ t_D = 3.146\ \mathrm{s}, V_{\rm rms} = 3.302\ \mathrm{km/s}, \alpha = 9.9^\circ, z_D = 10.454\ \mathrm{km}, x_D = 1.784\ \mathrm{km}. \end{align}
The use of any functional form involves approximation, so it is not surprising that values of the depths and horizontal displacements depend upon the way in which they are calculated.
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| Vertical depth calculations using velocity functions | Weathering corrections and dip/depth calculations |
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| Partitioning at an interface | Seismic velocity |
Also in this chapter
- Accuracy of normal-moveout calculations
- Dip, cross-dip, and angle of approach
- Relationship for a dipping bed
- Reflector dip in terms of traveltimes squared
- Second approximation for dip moveout
- Calculation of reflector depths and dips
- Plotting raypaths for primary and multiple reflections
- Effect of migration on plotted reflector locations
- Resolution of cross-dip
- Cross-dip
- Variation of reflection point with offset
- Functional fits for velocity-depth data
- Relation between average and rms velocities
- Vertical depth calculations using velocity functions
- Depth and dip calculations using velocity functions
- Weathering corrections and dip/depth calculations
- Using a velocity function linear with depth
- Head waves (refractions) and effect of hidden layer
- Interpretation of sonobuoy data
- Diving waves
- Linear increase in velocity above a refractor
- Time-distance curves for various situations
- Locating the bottom of a borehole
- Two-layer refraction problem