reflection seismology

The following books cover important topics in reflection seismology.

The concept of deconvolution had an early application in reflection seismology.

Reflection seismology has also found applications in non-commercial research by academic and government scientists around the world.

It is one of a number of seismic sources used in reflection seismology.

In common with other geophysical methods, reflection seismology may be seen as a type of inverse problem.

Reflection seismology identifies these layer boundaries by the reflections.

In reflection seismology, an array of seismometers image sub-surface features.

Reflection seismology profiles show the disturbed rock that hides a blind thrust fault.

For more information, see Reflection seismology.

Reflection seismology is similar to sonar and echolocation.

The survey using this method is very different from the conventional survey that is usually based on reflection seismology.

Petroleum industry basin analysis is often conducted on subterranean basins through the use of reflection seismology and data from well logging.

He patented the basic ideas leading to reflection seismology, a technique important for its use in exploring for petroleum.

The majority of geophones are used in reflection seismology to record the energy waves reflected by the subsurface geology.

Seismic inverse Q filtering is a data processing technology for enhancing the resolution of reflection seismology images.

The term and concept of exploding reflectors in reflection seismology is often attributed to Jon Claerbout.

Recently, the availability of cheap and high quality 3D seismic data (from reflection seismology) has greatly aided the accuracy of such interpretation.

Very high resolution seismics (reflection seismology) is applied to make detailed acoustic profiles of a sea floor or lake floor.

In reflection seismology, stacking velocity is the value of velocity obtained from the best-fit hyperbola analysis.

The Maud field, discovered in 1927 by Amerada Petroleum, was the first discovery using reflection seismology.

Seismic methods, such as reflection seismology, seismic refraction, and seismic tomography.

Using reflection seismology, this documentary demonstrated techniques that what Sarmast interpreted to be artificial walls are natural tectonic landforms.

For hydrocarbon exploration, MT is mainly used as a complement to the primary technique of reflection seismology exploration.

Shallower reflections are used in reflection seismology to study the Earth's crust generally, and in particular to prospect for petroleum and natural gas deposits.

Reflection seismology is used extensively in a number of fields and its applications can be categorised into three groups, each defined by their depth of investigation: