The generation of a seismic signal where compressional waves are completely absent is known to be a challenging task with shallow seismic surveys carried out in SH waves. This is true even when using appropriate source systems and taking the appropriate measures to prevent this from occurring. There are several factors that contribute to such issues including inclined energizing surfaces, oblique impact angles and the burial of the source system due to repetition of the shots. The presence of compressional waves is generally considered a serious problem in all SH waves investigations but it becomes a severe problem with reflection seismic surveys. In fact, amplification of the signal becomes a necessity with significant depths of investigat...
The primary focus of most reflection seismic surveys is to help locate hydro-carbon recourses. Due t...
In sites where earthquakes occur, the use of surface wave methods represents a convenient and effect...
SH-waves (Shear Horizontal) are often assumed to be decoupled from the other wave types (P-(Pressure...
Geophysical exploration measurements are used to obtain an image of the geological structures of the...
Seismic surveys are used to create visual representations of subsurface geology by detecting the ref...
Abstract the density and seismic velocity of the medium, changes in either of which can cause a refl...
High-resolution shallow seismic reflection surveys require more attention to the choice of source an...
Both architecture and physical properties of near-surface point-bar sediment packages have not be im...
Multicomponent seismic recording (measurement with vertical- and horizontal-component geophones and ...
Shallow seismic reflection survey is a powerful tool in revealing subsurface geometry of unstable sl...
The current project is a continuation of an effort to develop ultrashallow seismic imaging as a cost...
For civil structures founded on shallow foundations, the ground underneath the foundation often hold...
Copyright © 2003 Australian Society of Exploration GeophysicistsWe have developed a new full-wavefor...
Shallow seismic methods have historical roots dating to the 1930s, when limited shallow refraction w...
Seismic and electromagnetic imaging methods both provide the geophysicist with different types of me...
The primary focus of most reflection seismic surveys is to help locate hydro-carbon recourses. Due t...
In sites where earthquakes occur, the use of surface wave methods represents a convenient and effect...
SH-waves (Shear Horizontal) are often assumed to be decoupled from the other wave types (P-(Pressure...
Geophysical exploration measurements are used to obtain an image of the geological structures of the...
Seismic surveys are used to create visual representations of subsurface geology by detecting the ref...
Abstract the density and seismic velocity of the medium, changes in either of which can cause a refl...
High-resolution shallow seismic reflection surveys require more attention to the choice of source an...
Both architecture and physical properties of near-surface point-bar sediment packages have not be im...
Multicomponent seismic recording (measurement with vertical- and horizontal-component geophones and ...
Shallow seismic reflection survey is a powerful tool in revealing subsurface geometry of unstable sl...
The current project is a continuation of an effort to develop ultrashallow seismic imaging as a cost...
For civil structures founded on shallow foundations, the ground underneath the foundation often hold...
Copyright © 2003 Australian Society of Exploration GeophysicistsWe have developed a new full-wavefor...
Shallow seismic methods have historical roots dating to the 1930s, when limited shallow refraction w...
Seismic and electromagnetic imaging methods both provide the geophysicist with different types of me...
The primary focus of most reflection seismic surveys is to help locate hydro-carbon recourses. Due t...
In sites where earthquakes occur, the use of surface wave methods represents a convenient and effect...
SH-waves (Shear Horizontal) are often assumed to be decoupled from the other wave types (P-(Pressure...