Seismic methods
The geostack team has unique expertise in seismic applied to near-surface settings. With an acquisition system designed specifically by its technical team and inspired by university research, we have participated in a large number of characterization projects at different scales for industrial, academic and government partners. We are equipped for projects of all sizes and are very agile in adapting to your needs and meeting your objectives.

Rapid deployment


Deployment of three-component towed geophones

Can be used with an accelerated mass or a vibrating source

Yield up to 3 km/day on motorable road

Summer and winter operation

Used for seismic reflection and MASW2D surveys
Flexible deployment

Use of regular or accelerated sledgehammer, or dynamite as needed

Deployment of up to 48 measurement stations for seismic refraction or MASW surveys

Deployment of up to 156 three-component wireless stations for high-resolution combined seismic

Operation summer and winter, in all types of environment

Seismic refraction

Ideal for sites with unconsolidated deposits <20m thick

Allows bedrock surface mapping

Provides clues about the presence of fluid and the quality of the rock

Layer or tomography interpretation of Vp velocities

Seismic reflection

Ideal for depths 10 - 100 m

Often used for bedrock mapping

Allows mapping of Vs

Allows to differentiate the types of unconsolidated deposits (ex: sand vs clay)

MASW-1D

Provides a vertical profile of Vs for the site investigated

Deployment possible in urban or remote areas

Possibility of coupling with another seismic method to increase control over interpretation

MASW - 2D

Ideal for depths 0 – 30m

Allows mapping of stratigraphic units

Can be produced at the same time as seismic reflection

Useful for hydrogeological and geotechnical characterization

Vertical seismic profile ( downhole )

Deployment in an existing borehole

Allows high vertical resolution of seismic velocities P and S

Use of a three-component sensor for better identification of propagation modes
