汾渭地震带

应用极值理论对汾渭地震带地震危险性的估计

An Application of Statistical Theory of Extreme Values to the Estimation of the Earthquake Risk of the Fen-Wei Seismic Belt

汾渭地震带的b值和年平均发生率的研究

Study on b Value and Average Annual Incidence of Earthquakes in Fen-wei Seismotectonic Zone

本文用韦布尔（Weibull）分布对陕西省及汾渭地震带的中强地震活动进行概率统计分析，得到所研究地区的中强地震平均复发周期和发震概率。

In this paper , the average recurrence period and probability of moderately strong earthquake in shaanxi province and Fen & Wei seismic belt are obtained using Weibull distribution .

本文以汾渭地震带为例和以小震P、S振幅比测定的震源参数尝试应用了用小震断层面解反演区域平均应力场的方法。

In this paper , taking the Fen & wei seismic belt for example , and using the amplitude ratio of P 、 S to determine the seismic source parameters , it was inversed regional mean stress field by using the fault planes of small earthquake .

汾渭地震带地震发生的统计分析

Statistical analysis on the earthquake occurrence in FEN-WEI seismic zone

陕西省及汾渭地震带的发震概率

A study on probability of moderately strong earthquakes occurence in Shaanxi Province and fen & wei seismic belt

汾渭地震带Ms≥6级地震的可公度特征初探及中强地震节律分析

Approach on the commensurable character of m_s ≥ 6 earthquake on FEN-WEI seismic zone and the rhythm of moderate shocks

汾渭地震带Ms≥6级地震在时间上具有可公度性，可公度值为4.09年。

The Ms ° 6 . 0 earthquake on Fen-Wei seismic zone is of commensurability in time series . The commensurable value is equal to 4 . 09 years .