Title: Natural stone assessment with ground penetrating radar GPR
1Natural stone assessment with ground penetrating
radar (GPR)
- The 15th Meeting of the Association of European
Geological Societies - 1620 September 2007
- Tallinn, Estonia
2Natural stone assessment with ground penetrating
radar (GPR)
- Location of the study areas
3Natural stone assessment with ground penetrating
radar (GPR)
- The ground penetrating radar instrumentation
- GSSI SIR 2000 control unit
- Antennae between 40 MHz and 400 MHz
200 MHz antenna
Control unit
4Natural stone assessment with ground penetrating
radar (GPR)
- Porphyritic granite situated in the south-eastern
Finland - It belongs to the Central Finland granitoid
complex and is described - postkinematic in relation to the deformation of
the area
5Natural stone assessment with ground penetrating
radar (GPR)
6Natural stone assessment with ground penetrating
radar (GPR)
- Study area 1
- Typical feature of the rock is a strong
horizontal exfoliation type fracturing (height of
the bench about 5 m)
7Natural stone assessment with ground penetrating
radar (GPR)
- GPR measurement traverse of 65 m in length
(vertical and horizontal scale are equal) - The profile was corrected with altitude data to
present the actual surface and fractures
orientation
8Natural stone assessment with ground penetrating
radar (GPR)
- The GPR was able to detect the major horizontal
and sub-horizontal fracturing
9Natural stone assessment with ground penetrating
radar (GPR)
- Vertical or near vertical fractures were
difficult to detect due to their small reflection
surface towards the measuring antenna
10Natural stone assessment with ground penetrating
radar (GPR)
- The horizontal fractures near the surface were
sometimes strongly weathered providing space for
surface water to collect - Those spots were detected as individual targets
on the radar measurement profile - The spots can be thought to be reflections from a
sub-horizontal fracture zone near the surface
11Natural stone assessment with ground penetrating
radar (GPR)
Soapstone situated in North Karelia It belongs to
an Archaean greenstone belt, in the border zone
between the Archaean area and the
Palaeoproterozoic North Karelian Schist Belt
12Natural stone assessment with ground penetrating
radar (GPR)
Typical North Karelian soapstone Sample size 260
mm x 200 mm
13Natural stone assessment with ground penetrating
radar (GPR)
Soapstone quarry in North Karelia
14Natural stone assessment with ground penetrating
radar (GPR)
- With the soapstone, the measurements revealed
more of the internal structure of the rock,
making the detection of the fracturing complex - Especially internal lineation was quite well
visible in those sections where the stone
contained more conductive minerals.
15Natural stone assessment with ground penetrating
radar (GPR)
- Large open horizontal fractures were detectable
also in this stone type, which can be helpful in
planning of the quarrying operations.
16Natural stone assessment with ground penetrating
radar (GPR)
- Ground penetrating radar (GPR) is suitable for
large-scale quality assessment of natural stone
deposits and quarries - The measurements are easy and quick to do and the
preliminary results can be evaluated immediately - The fracture detection level varies depending on
the used equipment, mainly on the frequency - The development in GPS technology has made it
possible to position the measurements accurately
and thus trace back the results into the quarry
to help extraction planning - The differences in the measurement results and
their interpretation found among these two rock
types indicate the importance of knowing the
electromagnetic properties and mineralogy of the
stone - Also knowing the geological structure and other
characteristics of the stone beforehand helps to
avoid false interpretations