Q: What is Seismic?[+]
A: It is a method of determining sub-surface information by analyzing sound waves originating from an energy source.
Q: What is an energy source?[+]
A: The energy source is typically either a small amount of dynamite in a shot hole, drilled to depths of five to 150 feet or vibrations generated from a series of vibroseis trucks.
Q: How are the sound waves collected?[+]
A: The reflected sound waves are detected by listening devices called geophones that are laid out along the seismic line. Geophones are usually attached to cables that connect into a recording truck/doghouse where the seismic data is recorded.
Q: What is the difference between 2D & 3D?[+]
A: 2D seismic lines are single lines of regularly spaced geophone stations (e.g. every 55 feet). Energy source points are established along the line typically at every second or third station. The same line contains recording cables and geophones as well as source points.
3D seismic programs are generally a uniform and evenly spaced grid of lines. Receiver lines containing the recording devices (geophones) usually, but not always, run in a direction perpendicular or diagonal to the source lines. The spacing between lines can vary from project to project. Spacing between energy source points will also vary from project to project.