使用黏性逼近方法推广一个平衡及不动点问题

为了研究寻找一般平衡问题的公共解集中共有元素的迭代方法,及无穷非扩张映像族的不动点问题.通过在Hilbert空间中构造非扩张序列Ti得出了一种关于Wn算子的新黏性逼近迭代算法,在一定条件下,得出了其强收敛定理.     

开发区集约节约用地访谈(二) 宁乡经开区的两柄利剑

合理规划与严格监管,实际上正是从"开源"与"节流"两个最重要的节点上卡住了对土地的有效开发利用,宁乡经济开发区所有的集约节约用地思路和具体方法都可以归结到这两个方面。     

中国大陆地震空区统计特征分析

对中国大陆具备相对完整资料的367次5级以上地震,分5个工作片区进行统一定性要求的地震空区图像扫描,得到194次震前的空区图像.其中震前有空区地震与研究地震的比例分别为:华北片区14∶36;华东南片区21∶24;川滇片区68∶124;青藏高原北部片区36∶82;新疆片区55∶101.震前出现空区图像比例最低的为华北地区,最高的为华东南地区,新疆与川滇地区基本相当.在此基础上着重讨论了空区形成后发生的主震与空区形成持续时间、空区空间分布尺度及围空地震震级等的统计关系.结果表明,空区的持续时间、空间尺度与主震震级间存在一定的相关关系,但其误差较大.而围空的起始震级在5级主震前为ML2.5左右,6级主震前为ML3.5左右,7级以上主震前为ML4.0左右.主震通常发生在空区的边缘及附近的外部地区.5级、6级和7级地震前出现空区图像的比例分别为45.8%、72.6%和100%,一定程度上表明了震前空区图像是强震前的重要异常判据.     

用经验格林函数法模拟2008年日本岩手-宫城地震的强地面运动l

运用经验格林函数方法,对2008年6月13日日本岩手——宫城（MW 6.9）地震进行了近场强地面运动的模拟研究.首先,利用震源谱拟合方法和遗传优化算法计算了经验格林函数法所需的参数,进而估算求得了此次地震主断层面上强震生成区的面积和上升时间.基于所获得的震源模型,计算了近震源区域的强地面运动时程,并同实际观测记录在时域和频域作了分析比较.结果显示,多数台站合成谱与观测谱符合得很好,部分台站两者在低频上有一定的偏差.通过遗传算法搜寻,所得强震生成区的面积与经验关系预测的一致,而上升时间则比经验关系预测的要小.      

甘肃民勤地区新增加的几次中强历史地震

在甘肃省民勤地区进行历史地震资料考证和野外实地调查过程中,从新获得的《镇番遗事历鉴》等文献中新发现了6次中强历史地震的史料。根据综合分析及类比的原则和方法初步确定了各次地震的基本参数,为分析该地区的地震构造活动提供了新的资料。     

Study on the Anomaly of Small Earthquake Activity Before Moderate-strong Earthquake in the Northeast Margin of the Qinghai- Xizang （Tibet） Block

26 earthquakes with MS ≥5. 0 have been recorded in the northeast margin of the Qinghai- Xizang (Tibet) block since 1980,22 of which were relatively independent of other moderate- strong earthquakes. Research on the increase of small earthquake activity before the 22 moderate-strong earthquakes has indicated that small earthquake activity was enhanced before 17 of the moderate-strong earthquakes. Though the increased seismicity is a common phenomenon in the northeast margin of the Qinghai-Xizang ( Tibet ) block,we have difficulty in predicting the moderate-strong earthquakes by this phenomenon. In order to predict the moderate-strong earthquakes through the increased seismicity of small earthquakes,this paper attempts to propose a new method, which calculates small earthquake frequency through the change of distribution pattern of small earthquakes, based on the characteristics of small earthquake activity in the northeastern Qinghai-Xizang (Tibet) block,and then make primary applications. The result shows that we are able to obtain obvious anomalies in the frequency of small earthquakes before moderate strong earthquakes through the new method,with little spatial range effect on the amplitude of this small earthquake frequency anomaly. We can obtain mid to short-term anomaly indices for moderate-strong earthquakes in the northeast margin of the Qinghai-Xizang (Tibet) block.     

Influence of Surrounding Large Earthquakes on Moderate Earthquake Activity within Xinjiang

Based on the statistical results of the relationship between the large earthquakes surrounding Xinjiang and moderate earthquakes within Xinjiang since 1950, this article calculates the Coulomb failure stress change produced by the three groups of large earthquakes surrounding Xinjiang during the large earthquake active period outside Xinjiang and the quiet period inside Xinjiang from 1976 to 2007, and analyzes Xinjiang's moderate earthquake activity features in the three years after the large earthquakes surrounding Xinjiang.It then discusses the influence of large earthquake activity surrounding Xinjiang on seismic activity within Xinjiang. The research results show that the large earthquake activity surrounding Xinjiang may to a certain extent slow down the preparation process of moderate earthquakes in Xinjiang.     

Analysis of Digital Strong Motion Records of the M_S 8.0 Wenchuan Earthquake by the Network of Shaanxi Province

Records of the May 12,2008 MS8.0 Wenchuan,Sichuan,earthquake from 27 stations of Shaanxi Digital Strong Motion Network are processed and analyzed,including baseline adjustment of acceleration traces,filtering,and calculations of velocities,displacements and acceleration response spectra.The results show that direction energy radiation of the large earthquake and horizontal inhomogeneous medium along the wave traveling path might both have some effect on the scattering degree of the attenuation of PGAH,besides influence of local site conditions.For the same intensity,the ratios of PGA /PGV are commonly small,on average about 5,which indicates that long period components are rich in ground motion.Intensities for most sites of the stations are within Ⅴ～Ⅶ.The larger one among PGAE-W and PGAN-S is quite close to their PGAH,which is less than 10% in relative deviation.The dominated waves are surface waves.The thicker the soil overburden is,the stronger the surface wave will be and the longer the shaking will last.Local site conditions have strong effects on ground motion,especially those of thick sediment filled-in basins,as they can significantly amplify long-period components.     

中强地震空间分布“X”图像及其含义

基于西太平洋板块向欧亚大陆板块下俯冲产生的推挤,造成黑龙江亚板块地下的地幔物质上涌,使其上覆岩石圈受到垂直方向上涌力的作用。通过分析"X"节理的形成、与断层的关系、火山群"X"型断裂构造的特点,对黑龙江亚板块1999年以来中强地震空间分布进行研究,呈网格化特征分布。根据构造类比法和历史地震比拟法,网格化交汇处缺震区未来几年或更长时间存在发生中强地震的背景,即内蒙古扎兰屯,通辽和黑龙江五大连池,绥化历史老震区;尤其是2008年6月10日内蒙古扎兰屯附近(阿荣旗境内)发生M 5.2地震后该地区可能再次成为未来地震的危险区。本文研究结果对区域地震危险区的判定有借鉴意义。     

基于CDMA1X/GPRS网络采用VPN技术组建强地震观测网络系统

详细介绍了采用CDMA1X/GPRS网络组建天津市强地震观测VPN网络的技术流程与要点。通过该网络的组建,使天津强地震观测网络实现了自动监控、数据自动汇集、参数自动获取等功能,提高了天津强地震观测的自动化水平和管理水平,为天津市的震后灾害快速评估、应急及快速救援提供了技术保障,充分发挥了强地震观测在天津市防震减灾事业中的作用。