Ground roll attenuation using (f, k) and agora filters

Abstract

The seismic method is the most used method to capture and study the subsurface. The discipline of subsurface seismic imaging, or mapping the subsurface using seismic waves, takes a remote sensing approach to probe the Earth’s interior.The seismic method goes over three major phases: data acquisition, processing, and the interpretation processes. During the process of the acquisition and the transmission, the data is often corrupted by the different types of noises. Throughout our work, we focused on the study of the two dimensions’ filters (f, k) and AGORA.