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Integration of in-mine seismic and GPR surveys to gain advanced knowledge of Bushveld Complex orebodies

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dc.contributor.author Onyebueke, EO
dc.contributor.author Manzi, MSD
dc.contributor.author Rapetsoa, MK
dc.contributor.author Kgarume, Thabang E
dc.contributor.author Westgate, M
dc.contributor.author Durrheim, RJ
dc.contributor.author Pienaar, M
dc.contributor.author Sihoyiya, M
dc.contributor.author Mpofu, Mvikel
dc.contributor.author Van Schoor, Abraham M
dc.date.accessioned 2023-11-14T09:43:15Z
dc.date.available 2023-11-14T09:43:15Z
dc.date.issued 2023-08
dc.identifier.citation Onyebueke, E., Manzi, M., Rapetsoa, M., Kgarume, T.E., Westgate, M., Durrheim, R., Pienaar, M. & Sihoyiya, M. et al. 2023. Integration of in-mine seismic and GPR surveys to gain advanced knowledge of Bushveld Complex orebodies. <i>Near Surface Geophysics.</i> http://hdl.handle.net/10204/13203 en_ZA
dc.identifier.issn 1569-4445
dc.identifier.issn 1873-0604
dc.identifier.uri https://doi.org/10.1002/nsg.12270
dc.identifier.uri http://hdl.handle.net/10204/13203
dc.description.abstract Improving the exploration of deep-seated mineral deposits and assessing the stability of the mine pillars require that geophysical techniques are deployed in a fast and cost-effective manner with minimal environmental impact. This research presents results from in-mine reflection seismic experiments and a ground penetrating radar (GPR) survey conducted at the Maseve platinum mine, South Africa. The research aims to develop and implement methods to image platinum group metal (PGM) deposits and geological structures near mine tunnels and assess the stability of pillars. The seismic experiments were conducted using a sledgehammer source (10 lb), conventional cabled geophones (14 Hz), and a landstreamer with 4.5 Hz vertical component geophones. The GPR survey was conducted using a Noggin 500 GPR system with 500 MHz centre frequency. An image of the underlying orebody and geological structures down to 100 m from the mine tunnel floor (~500 m below ground surface) was produced. We correlated the coherent reflections beneath the tunnel floor with a known Upper Group (UG2) PGM orebody. The final seismic section shows that the UG2 mineralisation is dissected by near-vertical dykes, faults and fractures. These structures, faults in particular, are interpreted to have been active post-mineralisation, implying that they may have contributed to the current complex geometry of the deposit. Four GPR profiles were collected around a stability pillar adjacent to the seismic lines. The radargram sections were processed to improve the signal-to-noise ratio (S/N). The results show different patterns of fracturing and stress-induced structures. These fractures were shown to be sub-vertical and, possibly, constitute complex micro-structures within the pillar, which could compromise the pillar stability and integrity. The study demonstrates that in-mine seismic and GPR surveys can be cost-effective and valuable for mineral exploration. en_US
dc.format Abstract en_US
dc.language.iso en en_US
dc.relation.uri https://onlinelibrary.wiley.com/doi/10.1002/nsg.12270 en_US
dc.source Near Surface Geophysics en_US
dc.subject Data processing en_US
dc.subject Ground Penetrating Radar en_US
dc.subject GPR en_US
dc.subject Mining en_US
dc.subject Near-tunnel floor en_US
dc.subject Reflection seismic en_US
dc.title Integration of in-mine seismic and GPR surveys to gain advanced knowledge of Bushveld Complex orebodies en_US
dc.type Article en_US
dc.description.pages 15pp en_US
dc.description.note Due to copyright restrictions, the attached PDF file only contains the abstract of the full text item. For access to the full text item, please consult the publisher's website: https://onlinelibrary.wiley.com/doi/10.1002/nsg.12270 en_US
dc.description.cluster Mining en_US
dc.description.impactarea Mining and Mineral Resources en_US
dc.identifier.apacitation Onyebueke, E., Manzi, M., Rapetsoa, M., Kgarume, T. E., Westgate, M., Durrheim, R., ... Van Schoor, A. M. (2023). Integration of in-mine seismic and GPR surveys to gain advanced knowledge of Bushveld Complex orebodies. <i>Near Surface Geophysics</i>, http://hdl.handle.net/10204/13203 en_ZA
dc.identifier.chicagocitation Onyebueke, EO, MSD Manzi, MK Rapetsoa, Thabang E Kgarume, M Westgate, RJ Durrheim, M Pienaar, M Sihoyiya, Mvikel Mpofu, and Abraham M Van Schoor "Integration of in-mine seismic and GPR surveys to gain advanced knowledge of Bushveld Complex orebodies." <i>Near Surface Geophysics</i> (2023) http://hdl.handle.net/10204/13203 en_ZA
dc.identifier.vancouvercitation Onyebueke E, Manzi M, Rapetsoa M, Kgarume TE, Westgate M, Durrheim R, et al. Integration of in-mine seismic and GPR surveys to gain advanced knowledge of Bushveld Complex orebodies. Near Surface Geophysics. 2023; http://hdl.handle.net/10204/13203. en_ZA
dc.identifier.ris TY - Article AU - Onyebueke, EO AU - Manzi, MSD AU - Rapetsoa, MK AU - Kgarume, Thabang E AU - Westgate, M AU - Durrheim, RJ AU - Pienaar, M AU - Sihoyiya, M AU - Mpofu, Mvikel AU - Van Schoor, Abraham M AB - Improving the exploration of deep-seated mineral deposits and assessing the stability of the mine pillars require that geophysical techniques are deployed in a fast and cost-effective manner with minimal environmental impact. This research presents results from in-mine reflection seismic experiments and a ground penetrating radar (GPR) survey conducted at the Maseve platinum mine, South Africa. The research aims to develop and implement methods to image platinum group metal (PGM) deposits and geological structures near mine tunnels and assess the stability of pillars. The seismic experiments were conducted using a sledgehammer source (10 lb), conventional cabled geophones (14 Hz), and a landstreamer with 4.5 Hz vertical component geophones. The GPR survey was conducted using a Noggin 500 GPR system with 500 MHz centre frequency. An image of the underlying orebody and geological structures down to 100 m from the mine tunnel floor (~500 m below ground surface) was produced. We correlated the coherent reflections beneath the tunnel floor with a known Upper Group (UG2) PGM orebody. The final seismic section shows that the UG2 mineralisation is dissected by near-vertical dykes, faults and fractures. These structures, faults in particular, are interpreted to have been active post-mineralisation, implying that they may have contributed to the current complex geometry of the deposit. Four GPR profiles were collected around a stability pillar adjacent to the seismic lines. The radargram sections were processed to improve the signal-to-noise ratio (S/N). The results show different patterns of fracturing and stress-induced structures. These fractures were shown to be sub-vertical and, possibly, constitute complex micro-structures within the pillar, which could compromise the pillar stability and integrity. The study demonstrates that in-mine seismic and GPR surveys can be cost-effective and valuable for mineral exploration. DA - 2023-08 DB - ResearchSpace DP - CSIR J1 - Near Surface Geophysics KW - Data processing KW - Ground Penetrating Radar KW - GPR KW - Mining KW - Near-tunnel floor KW - Reflection seismic LK - https://researchspace.csir.co.za PY - 2023 SM - 1569-4445 SM - 1873-0604 T1 - Integration of in-mine seismic and GPR surveys to gain advanced knowledge of Bushveld Complex orebodies TI - Integration of in-mine seismic and GPR surveys to gain advanced knowledge of Bushveld Complex orebodies UR - http://hdl.handle.net/10204/13203 ER - en_ZA
dc.identifier.worklist 27194 en_US


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