The multichannel analysis of surface waves (MASW) seismic method was used to delineate a fault zone and gently dipping sedimentary bedrock at a site overlain by several meters of regolith. Seismic data were collected rapidly and inexpensively using a towed 30-channel land streamer and a rubberband-accelerated weight-drop seismic source. Data processed using the MASW method imaged the subsurface to a depth of about 20m20m and allowed detection of the overburden, gross bedding features, and fault zone. The fault zone was characterized by a lower shear-wave velocity (Vs)(Vs) than the competent bedrock, consistent with a large-scale fault, secondary fractures, and in-situ weathering. The MASW 2D VsVs section was further interpreted to identify dipping beds consistent with local geologic mapping. Mapping of shallow-fault zones and dipping sedimentary rock substantially extends the applications of the MASW method.
Additional publication details
|Publication Subtype||Journal Article|
|Title||Delineating a shallow fault zone and dipping bed rock strata using multichannal analysis of surface waves with a land streamer|
|Publisher||Society of Exploration Geophysicists|
|Contributing office(s)||Office of Ground Water, Toxic Substances Hydrology Program|
|Google Analytic Metrics||Metrics page|