Delay time
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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 | 11 |
| Pages | 415 - 468 |
| DOI | http://dx.doi.org/10.1190/1.9781560801733 |
| ISBN | ISBN 9781560801153 |
| Store | SEG Online Store |
Problem 11.8
Show that $ NQ $ in Figure 11.8a is given by
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} NQ=V_{2} \delta_{NQ} \tan ^{2} \theta_{c}, \\ \hbox{i.e.,}\quad \quad \delta _{g} =\delta _{NQ} =NQ/V_{2} \tan ^{2} \theta_{c}. \end{align} ()
Background
The concept of delay time has found wide application in refraction interpretation (see problems 11.9 and 11.11). We define the delay time associated with the refraction path SMNG in Figure 11.8a as the observed traveltime minus the time required to travel from 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/":): P to 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/":): Q at the velocity 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_{2} . $ PQ $ is the projection of the path SMNG onto the refractor), Writing 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/":): \delta for the total delay time, we have
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} \delta &=t_{SG} -PQ/V_{2} \end{align} ()
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} &=\left(\frac{SM+NG}{V_{1} } +\frac{MN}{V_{2} } \right)-\frac{PQ}{V_{2} } =\left(\frac{SM}{V_{1} } -\frac{PM}{V_{2} } \right)+\left(\frac{NG}{V_{1} } -\frac{NQ}{V_{2} } \right) \end{align}
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} &=\delta_{s} + \delta_{g}, \end{align} ()
$ {\begin{aligned}{\hbox{where}}\quad \quad \delta _{s}={\hbox{source delay time}}\ =\left({\frac {SM}{V_{1}}}-{\frac {PM}{V_{2}}}\right)\end{aligned}} $ ()
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} \hbox{and}\quad \quad \delta_{g} = \hbox{geophone delay time}\ = \left(\frac{NG}{V_{1} } -\frac{NQ}{V_{2} } \right). \end{align} ()
Solution
Referring to Figure 11.8a, we have, by definition,
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} \delta_{g} &=NG/V_{1} -NQ/V_{2} \\ &=NQ\left(\frac{1}{V_{1} \sin \theta _{c} } -\frac{1}{V_{2} } \right)=\frac{NQ}{V_{2} } \left(\frac{1}{\sin ^{2} \theta _{c} } -1\right)\\ &=NQ/V_{2} \tan ^{2} \theta _{c}. \end{align}
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| Proof of a generalized reciprocal method relation | Barry’s delay-time refraction interpretation method |
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| Geologic interpretation of reflection data | 3D methods |
Also in this chapter
- Salt lead time as a function of depth
- Effect of assumptions on refraction interpretation
- Effect of a hidden layer
- Proof of the ABC refraction equation
- Adachi’s method
- Refraction interpretation by stripping
- Proof of a generalized reciprocal method relation
- Delay time
- Barry’s delay-time refraction interpretation method
- Parallelism of half-intercept and delay-time curves
- Wyrobek’s refraction interpretation method
- Properties of a coincident-time curve
- Interpretation by the plus-minus method
- Comparison of refraction interpretation methods
- Feasibility of mapping a horizon using head waves
- Refraction blind spot
- Interpreting marine refraction data