Subsurface structures can thus be defined by the correlation of such properties.
The subsurface structures can then be probed from several different angles at the same time.
Telluric currents are often used by geophysicists to map subsurface structures, such as sedimentary basins, layered rocks, and faults.
When that happens, we'll have the capability to map the geoid and the subsurface structures that determine it with unprecedented accuracy.
Vice versa, these measurements may provide means to quantify hydromechanical effects caused by subsurface structures.
Airborne geophysical surveys enable us to clarify three-dimensional subsurface structures in large and inaccessible areas.
Hence a better detection of these subsurface structures is of great interest.
In such procedures, haptic detection of changing tissue properties at different depths during needle insertion is important for needle localization and detection of subsurface structures.
Over the next three to five years following the cruise, high-performance computers will be used to reconstruct detailed 3D images of the subsurface structures.
They enable one to probabilistically model subsurface structures in the form of a three-dimensional (3-D) probability field.
Ground-penetrating radar is a non-destructive geophysical technology that provides quantitative information about the subsurface structures.
