范强, 孟立朋, 张合, 温超, 杨歧炎, 吕国军. 河北地区空间分布函数的地质因子和中长期预报因子的计算[J]. 华北地震科学, 2013, 31(2): 35-38,45. DOI: 10.3969/j.issn.1003-1375.2013.02.007
引用本文: 范强, 孟立朋, 张合, 温超, 杨歧炎, 吕国军. 河北地区空间分布函数的地质因子和中长期预报因子的计算[J]. 华北地震科学, 2013, 31(2): 35-38,45. DOI: 10.3969/j.issn.1003-1375.2013.02.007
FAN Qiang, MENG Li-peng, ZHANG He, WEN Chao, YANG Qi-yan, LV Guo-jun. CALCULATION OF GEOLOGICAL FACTOR AND MID-AND LONG-TERM FORECAST FACTOR OF SPATIAL DISTRIBUTION FUNCTION IN HEBEI AREA[J]. North China Earthquake Sciences, 2013, 31(2): 35-38,45. DOI: 10.3969/j.issn.1003-1375.2013.02.007
Citation: FAN Qiang, MENG Li-peng, ZHANG He, WEN Chao, YANG Qi-yan, LV Guo-jun. CALCULATION OF GEOLOGICAL FACTOR AND MID-AND LONG-TERM FORECAST FACTOR OF SPATIAL DISTRIBUTION FUNCTION IN HEBEI AREA[J]. North China Earthquake Sciences, 2013, 31(2): 35-38,45. DOI: 10.3969/j.issn.1003-1375.2013.02.007

河北地区空间分布函数的地质因子和中长期预报因子的计算

CALCULATION OF GEOLOGICAL FACTOR AND MID-AND LONG-TERM FORECAST FACTOR OF SPATIAL DISTRIBUTION FUNCTION IN HEBEI AREA

  • 摘要: 利用华北平原地震带潜在震源区和河北省活动断裂资料,采用地质资料的定量化方法和中长期预报的震级-时间模型计算每个潜在震源区的地质因子和中长期预报因子。地质因子计算结果为:(1)地质因子最高的地区出现在唐山、北京、邢台、邯郸;(2)3类地区(全新世断裂活动、晚更新世断裂活动和无全新世或晚更新世断裂活动)的地质因子比值约为12:4:1。中长期预报因子采用邵辉成等人的研究成果,考虑历史地震和现代地震资料等不同精度的地震矩年变化率,其结果能代表长期的平均值,避免了使用部分平静期或活跃期的资料而掩盖长期地震活动的真实情况,从而减少结果的不确定性。

     

    Abstract: Based on the data of latent focal region in North China seismic belt and active faults in Hebei Province, the geological factor and mid-and long-term forecast factor were determined by using the quantity method of geological data and magnitude-time model of mid-and long term prediction.The geological factor show (1) the highest values in Tangshan, Beijing, Xingtai and Handan;(2) the ratio of geological factor in three types region(Holocene, late Pleistocene and no Holocene or late Pleistocene fault activity) is about 12:4:1.The mid-and long-term forecast factor use the result of Shao Huicheng et al, considering the historical earthquakes and modern seismic data, the annual change rate of seismic moment can represent the long-term average, which can avoid the situation of obscure the real long-term seismicity by using the data of inactive or active period and reduce the the uncertainty of the results.

     

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