Frequency -magnitude distribution of -3.7 < Mw <1 mining-induced earthquakes around a mining front and b value invariance with post-blast time
Frequency -magnitude distribution of -3.7 < Mw <1 mining-induced earthquakes around a mining front and b value invariance with post-blast time
复制标题
采矿前缘周围-3.7 < Mw <1 采矿诱发地震的频率震级分布以及 b 值随爆炸后时间的不变性
DOI:
10.1007/s00024-013-0721-7
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发表时间:
2013
影响因子:
2
通讯作者:
and H. Ogasawara
中科院分区:
文献类型:
--
作者:
Naoi;M.;M. Nakatani;S. Horiuchi;Y. Yabe;J. Philipp;T. Kgarume;G. Morema;S. Khambule;T. Masakale;L. Ribeiro;K. Miyakawa;A. Watanabe;K. Otsuki;H. Moriya;O. Murakami;H. Kawakata;N. Yoshimitsu;A. Ward;R. Durrheim;and H. Ogasawara
We 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 toMW−5. When records of blasts were removed, FMDs of AEs obeyed a Gutenberg−Richter law with similarbvalues, 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 (RichardsonandJordanBull 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 withb∼ 1.2 was valid betweenMW−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 samebvalue up toMW1.