Abstract
Summary This study presents the new data from the faults within Upper Pleistocene-Holocene deposits, presented by pebbles, cobbles, and boulders with a coarse-medium sandy matrix. Such sediments produce complex and diffuse wave patterns on GPR data, and it is challenging to recognise the faulting among them. Thus, we solved the direct problem of detecting fault zone features by GPR using numerical modelling. Comparing numerical simulation results with field data (GPR profiles and trench wall sketches), we proposed a summary of signs of the fault zone on GPR profiles.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.