Fault Detection with Crosshole and Reflection Geo-Radar for Ungerground Mine Safety
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in: Geosciences, Jahrgang 10.2020, Nr. 11, 456, 12.11.2020.
Publikationen: Beitrag in Fachzeitschrift › Artikel › Forschung › (peer-reviewed)
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TY - JOUR
T1 - Fault Detection with Crosshole and Reflection Geo-Radar for Ungerground Mine Safety
AU - Kulich, Jakob
AU - Bleibinhaus, Florian
N1 - Publisher Copyright: © 2020 by the authors. Licensee MDPI, Basel, Switzerland.
PY - 2020/11/12
Y1 - 2020/11/12
N2 - Ground-penetrating radar and crosshole radar are applied in an underground marble mine for fault detection and to test if different geological bodies can be distinguished. Boreholes are often drilled in advance of mining to clarify the locations of ore bodies and gangues. Here, such boreholes were used for crosshole investigations to supplement optical borehole imaging. Four boreholes were drilled along a profile with increasing offsets from 5 to 25 m. The crosshole measurements were performed with 100 MHz antennas. Tomographic panels were created up to a depth of 28 m and were complemented by reflection mode ground-penetrating radar (GPR) measurements along a 25 m-long profile with 100 and 250 MHz antennas. The GPR imaging successfully delineates the fault and karstification zones with higher water content due to their strong dielectric permittivity contrast compared to the surrounding geology.
AB - Ground-penetrating radar and crosshole radar are applied in an underground marble mine for fault detection and to test if different geological bodies can be distinguished. Boreholes are often drilled in advance of mining to clarify the locations of ore bodies and gangues. Here, such boreholes were used for crosshole investigations to supplement optical borehole imaging. Four boreholes were drilled along a profile with increasing offsets from 5 to 25 m. The crosshole measurements were performed with 100 MHz antennas. Tomographic panels were created up to a depth of 28 m and were complemented by reflection mode ground-penetrating radar (GPR) measurements along a 25 m-long profile with 100 and 250 MHz antennas. The GPR imaging successfully delineates the fault and karstification zones with higher water content due to their strong dielectric permittivity contrast compared to the surrounding geology.
UR - http://www.scopus.com/inward/record.url?scp=85096050303&partnerID=8YFLogxK
U2 - https://doi.org/10.3390/geosciences10110456
DO - https://doi.org/10.3390/geosciences10110456
M3 - Article
VL - 10.2020
JO - Geosciences
JF - Geosciences
SN - 2076-3263
IS - 11
M1 - 456
ER -