So.Ge.T company was created in 2008 by Simone Sartini
and Alessandro Bianchi who combined their expertise and their
professional knowledge to build a common goal: a young and
dynamic company capable of becoming a leader in the market
of applied geophysics. Their goal was to begin first in Italy then
build towards a future to serve foreign countries as well.

SEISMIC REFRACTION TOMOGRAPHY (SRT)
So.Ge.T has an extensive experience in conducting seismic
investigations, in a variety of environmental conditions.
The SRT method, widely used due to its versatility,
is by far the most important geophysical technique in every
engineering project.

GEOELECTRICAL RESISTIVITY TOMOGRAPHY
Geoelectrical tomography, the leading technique in geo-electrical
measurements, combines modern techniques of data acquisition
with performing interpretation solutions. It is based on the different
electrical property of the materials constituting the soil investigated.

Ground Penetrating Radar (also called georadar)
uses radio wave reflections (frequency from 25 MHz to 3,000 Mhz)
to collect information of underground or within a structure
such as buried pipes, underground cavities, subsurface cracks,
voids and layers’ thickness. The advantages of the method are clear:
GPR technology can locate any pipes/structures/objects:
metallic and nonmetallic (PVC, concrete, etc.).
It is a non-destructive and non-invasive test, revealing a wealth
of internal detail without the need for coring or breaking out
reducing associated risks and costs.

Magnetic surveys
So.Ge.T. Magnetic geophysical surveys are aimed at
measuring small, localised variations in the Earth's magnetic field.
The magnetic properties of naturally occurring materials such
as magnetic ore bodies and basic igneous rocks allows them to be
identified and mapped by magnetic surveys.

Topography is a branch of geodesy that deals with the
measurement technique of a portion of Earth’s shell,
aiming at representing how elements of an ensemble
are arranged in space. It is used to determine the
position of earth elements on small surfaces, as well as to obtaining
a graphical or numerical representation of the measured surfaces
(for drawing up maps and plans), detailed description of a place in terms
of placement, configuration, etc.