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.
Connecticut Geophysical and Seismic Operations
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US-OG-800
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The seismic survey is one form of geophysical survey that aims at measuring the earth's (geo-) properties by means of physical (-physics) principles such as magnetic, electric, gravitational, thermal, and elastic theories.
Types of Seismic Waves There are several different kinds of seismic waves, and they all move in different ways. The two main types of waves are body waves and surface waves. Body waves can travel through the Earth's inner layers, but surface waves can only move along the surface of the planet like ripples on water.
There are three major types of seismic surveys: refraction, reflection, and surface-wave depending on the specific type of waves being utilized.
The entire procedure for MASW usually con- sists of three steps: (1) acquiring multichannel field records (or shot gathers); (2) extracting dis- persion curves (one from each record); and (3) inverting these dispersion curves to obtain 1D (depth) VS profiles (one profile from one curve).
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.
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.
Active seismic methods can be divided into refraction and reflection methods. Refraction method, also called deep seismic sounding (DSS) or wide-angle reflection and refraction (WARR), consists of recording and interpreting refracted and reflected waves.
Abstract. The basic principle of all seismic methods is the controlled generation of elastic waves by a seismic source in order to obtain an image of the subsurface. Seismic waves are pulses of strain energy that propagate in solids and fluids.