Using Fresnel Zone to Characterise and Image Different Types of Diffractors in Low S/N Situations
Access Status
Authors
Date
2015Type
Metadata
Show full item recordCitation
Source Title
Source Conference
School
Collection
Abstract
We investigate the possibility to image and characterise the different types of diffractors – such as point, line, and edge – and separate them from reflections by limiting the aperture around the tangent point between the diffraction hyperbola and the relfection traveltime surface. To this end, we look at the tangents of the diffraction hyperbola with typical traveltime surfaces corresponding to the different diffrator types. We do this by studying the coherency of the recorded wavefield along the diffraction hyperbolae. The different types of diffractors show different energy distributions that can be used to characterise the diffractors and separate them from specular reflections. These areas of high energy correspond to the Fresnel zones of the particular diffractor type. Limiting the aperture of the diffraction hyperbola to the particular Fresnel zone results in improvement in S/N, while omitting the Fresnel zone corresponding to the reflections allows for imaging of the diffractors, which have larger Fresnels zones.
Related items
Showing items related by title, author, creator and subject.
-
Khoshnavaz, M Javad; Bóna, Andrej; Hossain, Muhammad; Urosevic, Milovan; Chambers, K. (2016)The primary objective of seismic exploration in a hard rock environment is the detection of heterogeneities such as fracture zones, small-scale geobodies, intrusions, and steeply dipping structures that are often associated ...
-
Malehmir, A.; Schmelzbach, C.; Bongajum, E.; Bellefleur, G.; Juhlin, Christopher; Tryggvason, A. (2009)2D crooked-line seismic reflection surveys in crystalline environments are often considered challenging in their processing and interpretation. These challenges are more evident when complex diffraction signals that can ...
-
Khoshnavaz, M.; Bóna, A.; Urosevic, Milovan (2017)Diffractions carry valuable information about local discontinuities and small-scale objects in the subsurface. They are still not commonly used in the process of geological interpretation. Many diffraction imaging techniques ...