# Mapping the vertical flank of a salt dome

Series | Geophysical References Series |
---|---|

Title | Problems in Exploration Seismology and their Solutions |

Author | Lloyd P. Geldart and Robert E. Sheriff |

Chapter | 13 |

Pages | 485 - 496 |

DOI | http://dx.doi.org/10.1190/1.9781560801733 |

ISBN | ISBN 9781560801153 |

Store | SEG Online Store |

## Contents

## Problem 13.6a

Two media of velocities and are separated by a vertical plane interface. A source is located at on the surface of the high-velocity medium and a geophone at point in a well in the other medium. If is the traveltime of a wave from to along the path *SAG* where is on the salt/sediment interface, discuss the locus of points located at the intersection of arcs centered at and having radii and , respectively, where .

### Solution

Any path where the interface is tangent to the locus curve satisfies the observed traveltime. To draw the locus we try a series of points such that . If a number of loci can be drawn for various geophone (or source) loctions, then their common tangent must locate the interface.

While this problem illustrates the concept, it can also be applied in three dimensions to allow for situations where and do not lie in the same plane.

500 | 0.44 | 1250 | 0.52 | 2000 | 0.6 |

750 | 0.46 | 1500 | 0.56 | 2250 | 0.67 |

1000 | 0.49 | 1750 | 0.60 | 2500 | 0.70 |

## Problem 13.6b

An outcropping salt dome has roughly vertical flanks. A source is located on the salt and a geophone is suspended in a vertical well in the sediments 1600 m from the source point. Determine the outline of the salt dome from the data in Table 13.6a. Take the velocities in the salt and adjacent sediments as 5.00 and 3.00 km/s.

### Solution

The usual method of resolving this problem is to prepare a vertical section through the well W and source point S, then draw a series of circles centered at S with radii equal to the distances traveled in salt for convenient time intervals such as 0.2 s, 0.4 s, etc., the circles being labeled with the time value. A second set of concentric circles using the sediment velocity is drawn on a transparency; the center of these circles is then placed over a geophone position, and intersections of the two sets of circles are marked wherever the time values of the two radii add up to give the traveltime to the geophone.

An alternative method is to dispense with the circles and use only the radii. The centers of the circles and the extremities of the radii are marked along the edges of two narrow strips of light cardboard (one for salt, one for sediments), the time values being marked as before (the marks and the centers should be on opposite sides of the two strips to permit accurate determinations of the intersections). Map pins can be used to attach the zero points of the two strips to the vertical section, one at the source point and the other at the geophone location in the well. Intersections are found as before and marked directly on the section. After curves have been plotted for each geophone position, the flank is outlined by the curve through the apices of the curves. The results are shown in Figure 13.6a.

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Effect of velocity change on VSP traveltime | Poission’s ratio from P- and S-wave traveltimes |

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3D methods | Specialized applications |

## Also in this chapter

- S-wave conversion in marine surveys
- Equally inclined orthogonal geophones
- Guided (channel) waves and normal-mode propagation
- Vertical seismic profiling
- Effect of velocity change on VSP traveltime
- Mapping the vertical flank of a salt dome
- Poission’s ratio from P- and S-wave traveltimes