Mississippi Seismic Data and Operations

State:
Multi-State
Control #:
US-OG-720
Format:
Word; 
Rich Text
Instant download

Description

This form is used when the Parties agree and shall contribute all proprietary seismic data and all non-proprietary seismic data affecting the Contract Area in its possession as of the effective date of this Agreement, to the extent the data is not restricted by confidentiality or licensing agreements with third parties. It is specifically understood and agreed that each Party has the right to sell, trade, and/or otherwise market seismic data involving the Contract Area which was in its possession prior to the effective date of this Agreement, and the benefits and advantages, including monetary consideration, which it receives as a result of those activities shall be the sole property of the party who owns the data.

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FAQ

There are three major types of seismic surveys: refraction, reflection, and surface-wave depending on the specific type of waves being utilized.

There are three types of seismic data: Reflection (including 2-D and 3-D) Shear wave. Refraction.

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.

There are three major types of seismic surveys: refraction, reflection, and surface-wave depending on the specific type of waves being utilized.

Seismic surveys use acoustic waves to create images of the earth through analysis of vibrations from those waves. Some seismic waves can penetrate solid rock and fluids into the deep inner layers of the earth, while others can only travel along the earth's surface, like ripples on water.

One of the most obvious differences between 2D and 3D seismic is that 3D imaging provides information continuously through the subsurface whereas 2D seismic reveals only strips of information. Nevertheless, 3D seismic may not be cost-effective in many onshore provinces, especially in the early stages of exploration.

Seismic surveys use reflected sound waves to produce a ?CAT scan? of the Earth's subsurface. Seismic surveys can help locate ground water, are used to investigate locations for landfills, and characterize how an area will shake during an earthquake, but they are primarily used for oil and gas exploration.

The refraction technique uses a long array of geophones to sense refracted waves, and the reflection technique uses a condensed array near the source to sense reflected waves (Fig. 4.10). Reflection surveys are widely used to map the upper crust for oil and gas exploration.

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Mississippi Seismic Data and Operations