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Frequency–magnitude distribution of -3.7 < M(subW) < 1 mining-induced earthquakes around a mining front and b value invariance with post-blast time

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dc.contributor.author Naoi, M
dc.contributor.author Nakatani, M
dc.contributor.author Horiuchi, S
dc.contributor.author Yabe
dc.contributor.author Philipp, J
dc.contributor.author Kgarume, Thabang E
dc.contributor.author Morema, G
dc.contributor.author Khambule, S
dc.contributor.author Masakele, T
dc.contributor.author Ribeiro, L
dc.contributor.author Miyakawa, K
dc.contributor.author Watanabe, A
dc.contributor.author Otsuki, K
dc.contributor.author Moriya, H
dc.contributor.author Murakami, O
dc.contributor.author Kawakata, H
dc.contributor.author Yoshimitsu, N
dc.contributor.author Ward, A
dc.contributor.author Durrheim, R
dc.contributor.author Ogasawara, H
dc.date.accessioned 2015-11-10T09:11:08Z
dc.date.available 2015-11-10T09:11:08Z
dc.date.issued 2014-10
dc.identifier.citation Naoi, M, Nakatani, M, Horiuchi, S, Yabe, Y, Philipp, J, Kgarume, T, Morema, G, Khambule, S, Masakele, T, Ribeiro, L, Miyakawa, K, Watanabe, A, Otsuki, K, Moriya, H, Murakami, O, Kawakata, H, Yoshimitsu, N, Ward, A, Durrheim, R and Ogasawara, H. 2014. Frequency–magnitude distribution of -3.7 < M(subW) < 1 mining-induced earthquakes around a mining front and b value invariance with post-blast time, Pure and Applied Geophysics, vol 171(10), pp 2665-2684 en_US
dc.identifier.issn 0033-4553
dc.identifier.uri http://link.springer.com/article/10.1007/s00024-013-0721-7
dc.identifier.uri http://hdl.handle.net/10204/8251
dc.description Copyright: 2014 Springer Basel. 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. The definitive version of the work is published in Pure and Applied Geophysics, Vol 171(10), pp 2665-2684 en_US
dc.description.abstract The authors investigated frequency-magnitude distribution (FMD) of acoustic emissions (AE) occurring near an active mining front in a South African gold mine, using a catalog developed from an AE network, which is capable of detecting AEs down to M(subW) -5. When records of blasts were removed, FMDs of AEs obeyed a Gutenberg-Richter law with similar b values, not depending on post-blasting time from the initial 1-min interval through more than 30 h. This result denies a suggestion in a previous study (RICHARDSON and JORDAN Bull Seismol Soc Am, 92:1766–1782, 2002) that new fractures generated by blasting disturb the size distribution of background events, which they interpreted as slip events on existing weak planes. Our AE catalog showed that the GR law with b * 1.2 was valid between M(subW) -3.7 and 0 for AEs around the mining front. Further, using the mine’s seismic catalog, which covers a longer time period of the same area, we could extend the validity range of the GR law with the same b value up to M(subW) 1. en_US
dc.language.iso en en_US
dc.publisher Springer Basel en_US
dc.relation.ispartofseries Workflow;14401
dc.subject Acoustic emission en_US
dc.subject Gutenberg Richter law en_US
dc.subject Mining-induced earthquake en_US
dc.title Frequency–magnitude distribution of -3.7 < M(subW) < 1 mining-induced earthquakes around a mining front and b value invariance with post-blast time en_US
dc.type Article en_US
dc.identifier.apacitation Naoi, M., Nakatani, M., Horiuchi, S., Yabe, Philipp, J., Kgarume, T. E., ... Ogasawara, H. (2014). Frequency–magnitude distribution of -3.7 < M(subW) < 1 mining-induced earthquakes around a mining front and b value invariance with post-blast time. http://hdl.handle.net/10204/8251 en_ZA
dc.identifier.chicagocitation Naoi, M, M Nakatani, S Horiuchi, Yabe, J Philipp, Thabang E Kgarume, G Morema, et al "Frequency–magnitude distribution of -3.7 < M(subW) < 1 mining-induced earthquakes around a mining front and b value invariance with post-blast time." (2014) http://hdl.handle.net/10204/8251 en_ZA
dc.identifier.vancouvercitation Naoi M, Nakatani M, Horiuchi S, Yabe, Philipp J, Kgarume TE, et al. Frequency–magnitude distribution of -3.7 < M(subW) < 1 mining-induced earthquakes around a mining front and b value invariance with post-blast time. 2014; http://hdl.handle.net/10204/8251. en_ZA
dc.identifier.ris TY - Article AU - Naoi, M AU - Nakatani, M AU - Horiuchi, S AU - Yabe AU - Philipp, J AU - Kgarume, Thabang E AU - Morema, G AU - Khambule, S AU - Masakele, T AU - Ribeiro, L AU - Miyakawa, K AU - Watanabe, A AU - Otsuki, K AU - Moriya, H AU - Murakami, O AU - Kawakata, H AU - Yoshimitsu, N AU - Ward, A AU - Durrheim, R AU - Ogasawara, H AB - The authors investigated frequency-magnitude distribution (FMD) of acoustic emissions (AE) occurring near an active mining front in a South African gold mine, using a catalog developed from an AE network, which is capable of detecting AEs down to M(subW) -5. When records of blasts were removed, FMDs of AEs obeyed a Gutenberg-Richter law with similar b values, not depending on post-blasting time from the initial 1-min interval through more than 30 h. This result denies a suggestion in a previous study (RICHARDSON and JORDAN Bull Seismol Soc Am, 92:1766–1782, 2002) that new fractures generated by blasting disturb the size distribution of background events, which they interpreted as slip events on existing weak planes. Our AE catalog showed that the GR law with b * 1.2 was valid between M(subW) -3.7 and 0 for AEs around the mining front. Further, using the mine’s seismic catalog, which covers a longer time period of the same area, we could extend the validity range of the GR law with the same b value up to M(subW) 1. DA - 2014-10 DB - ResearchSpace DP - CSIR KW - Acoustic emission KW - Gutenberg Richter law KW - Mining-induced earthquake LK - https://researchspace.csir.co.za PY - 2014 SM - 0033-4553 T1 - Frequency–magnitude distribution of -3.7 < M(subW) < 1 mining-induced earthquakes around a mining front and b value invariance with post-blast time TI - Frequency–magnitude distribution of -3.7 < M(subW) < 1 mining-induced earthquakes around a mining front and b value invariance with post-blast time UR - http://hdl.handle.net/10204/8251 ER - en_ZA


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