Inverting the head wave coefficient with multi-fold near-surface seismic refraction data

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Relationship between head wave amplitudes and seismic refraction velocities to detect lateral variation in the refractor

Refractor ambiguities are big problem in seismic refraction method especially in seismic engineering. There can be hidden subsurface geological phenomena such as hidden faults and shear zones which are not simply predicted by the travel-time graph or some geophysical methods. Head wave amplitudes are used to show the resolution of refractor ambiguities and the existence of anisotropy in complex...

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relationship between head wave amplitudes and seismic refraction velocities to detect lateral variation in the refractor

refractor ambiguities are big problem in seismic refraction method especially in seismic engineering. there can be hidden subsurface geological phenomena such as hidden faults and shear zones which are not simply predicted by the travel-time graph or some geophysical methods. head wave amplitudes are used to show the resolution of refractor ambiguities and the existence of anisotropy in complex...

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ژورنال

عنوان ژورنال: ASEG Extended Abstracts

سال: 2019

ISSN: 2202-0586

DOI: 10.1080/22020586.2019.12072941