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机构地区:[1]西北工业大学工程力学系
出 处:《地震地质》2006年第3期405-410,共6页Seismology and Geology
基 金:地震科学联合基金(103075;104016)资助。
摘 要:文中应用基于“多态”前兆模式及效能评价的最优效能单项模型参数选择方法,分析了3个地震带活断层(Qp3—Qh)与地震(M≥6)空间分布之间的关系。结果表明,河套地震带地震较集中分布在距断层20km的范围内,用其对6级以上地震进行地点预测有较高的准确性,R值达0.5,而对祁连山地震带30km范围内地震的发生地点进行预测,R值却仅为0.14。The gestation and occurrence of strong earthquake are closely related to fault activity, which are not only revealed by abundant experimentation and seismism but also proved by modern seismology. In the mainland of China, the correlation between earthquake activity and active fault is one of the bases for partitioning potential seismic sources, analyzing the seismotectonics and estimating location of strong earthquake. Due to nonuniformity of earth medium, instability of observation system and disturbance of environment etc, the variety of observational data is complicated, that is, there is no absolute "normal" or "abnormal", and seismic anomaly can be divided into many mutually exclusive "abnormal states". In different conditions of combined time-space-strength, determining the seismic anomaly by different monomial forecast method and its efficiency could be different due to the uncertainty of precursor itself or complexity of relation between precursor and earthquake gestation. In a "two-state" model, the difference could hardly be discovered and disposed in actual application. But in the "multi-state" model, the difference can be easily reflected and the optimal combination of forecasting parameters for a forecast method can also be determined easily. Based on the " multi-state" precursory model and the optimization method for parameters of earthquake forecast model under the condition of maximization of forecast efficiency, the relations of spatial location of earthquakes with M≥6 and active faults in three seismic belts are analyzed. The resuits demonstrate that in the Hetao Seismic Belt, seismicity is mostly concentrated in the range of 20km along the fault, the optimization model can forecast the location of potential earthquake of M≥6 near the faults with a relatively high accuracy, and the reliability value is 0.5 ; while in the Qilan Mt Seismic Belt, the reliability only reaches 0.14 when we use the model to estimate earthquakes within 30km range along the faults. T
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