Guam Geophysical and Seismic Operations

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US-OG-800
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This lease rider form may be used when you are involved in a lease transaction, and have made the decision to utilize the form of Oil and Gas Lease presented to you by the Lessee, and you want to include additional provisions to that Lease form to address specific concerns you may have, or place limitations on the rights granted the Lessee in the “standard” lease form.

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FAQ

Seismic acquisition requires the use of a seismic source at specified locations for a seismic survey, and the energy that travels within the subsurface as seismic waves generated by the source gets recorded at specified locations on the surface by what is known as receivers (geophones or hydrophones).

A critically refracted seismic wave travels along acoustic interfaces and generates new waves that can be detected at the surface. The seismic-refraction method measures the time a seismic-energy pulse takes to travel from a source point to several receivers after being redirected by one or more subsurface interfaces.

For a 3D seismic survey, a network of sensors in a grid is planted and a network of source points is located. The grid of receivers and source point is moved over the survey area as the survey progresses until the entire area is covered by the survey.

There are three phases of seismic surveys: data acquisition, processing, and interpretation. 3D surveys are acquired by laying out energy source points and receiver points in a grid over the area to be surveyed.

Seismic methods involve measuring the propagation of seismic waves through earth materials. In seismic surveys, seismic waves radiate outward from a sound source at the surface, which can be an explosive charge or a mechanical impact.

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Guam Geophysical and Seismic Operations