Mississippi Seismic Agreement Allowing Third Party to Conduct Seismic Operation on Grantor's Lease
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FAQ
Seismic interpretation conveys the geologic meaning of data by extracting subsurface information from it. Type of interpretation depends on the geologic objectives linked to the phase of exploration and on the kind of available data, 2D/3D, its grid density and quality.
There are three major types of seismic surveys: refraction, reflection, and surface-wave depending on the specific type of waves being utilized.
Seismic Refraction Procedure The seismic refraction method relies on travel times of sound waves, measured in milliseconds, traveling through and refracting from subsurface layers with contrasting densities. The seismic refraction lines will be surveyed using a Geometrics Geode, 24-channel seismograph.
Seismic or acoustic methods measure the travel times of the reflected or refracted waves detected by a series of geophones placed on the ground surface and are able to estimate the location and depth of the targets.
Seismic processing attempts to enhance the signal to noise ratio of the seismic section and remove the artifacts in the signal that were caused by the seismic method. The end result should be a more interpretable section. The process has some very subjective elements.