利用克里金技术标定新疆及附近地区P/S震相幅值比及其在地震事件识别中的应用
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摘要
针对中国的乌鲁木齐台(WMQ)和哈萨克斯坦的马坎奇台(MAK),采用贝叶斯克里金技术建立了新疆及附近地区地震事件的P/S震相幅值比的校正曲面,并分析了校正曲面与地震波传播路径的关系,以及校正曲面对于改善P/S震相幅值比判据识别效果的有效性.分析结果表明,建立的校正曲面基本合理,结合传播路径差异和地震波传播规律,能够较好地解释校正曲面的起伏特征.而且,在传播路径差异较大,使得P/S震相幅值比经震中距校正后离散度仍然较高的情况下,利用校正曲面修正P/S震相幅值比,可以进一步降低其离散度,从而改善判据的识别效果.MAK台lg[Pn(2~4Hz)/Lg(2~4Hz)]经校正曲面修正后,对天然地震的误识率由16.3%下降为5.2%.
Correction maps of P/S amplitude ratios for seismic events distributed in Xinjiang, China and adjacent areas were established using a Bayesian kriging method for the two seismic stations WMQ and MAK. The relationship between correction maps and variations of along-path features was analyzed and the validity of applying the correction maps to improve performances of P/S discriminants for seismic discrimination was investigated. Results obtained show that obtained correction maps in general may reflect event-station path effects upon corresponding P/S discriminants; and the correction of these effects could further reduce scatters of distance corrected P/S measurements within earthquake and explosion populations as well as improve their discriminating performances if path effects are a significant factor of such scatters. For example, as corresponding kriging correction map was applied, the misidentification rate of earthquakes by lg[Pn(2~4 Hz)/Lg(2~4 Hz)] at MAK was reduced from 16.3% to 5.2%.
引文
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