2004年阳江4.9级地震破裂方位角研究   总被引：2，自引：0，他引：2  

叶秀薇  闻则刚  邱奕超  杨马陵  刘吉平 《大地测量与地球动力学》2006,26(4):102-106

在一维有限移动震源模式下,根据地震波传播过程中的多普勒效应利用S波或P波拐角频率的方向性来确定地震破裂面的方法,计算了2003年11月~2005年10月阳江地区13次ML≥2.5地震的发震断层走向,结果显示:利用S波、P波拐角频率得到的2004年9月阳江4.9级地震破裂方位角分别为167°和166°,地震序列以NNW为主要破裂方向。  相似文献   

江苏省土地利用变化及其驱动机理研究   总被引：5，自引：2，他引：3  

谭少华  倪绍祥  赵万民 《地理与地理信息科学》2006,22(5):50-54

基于土地利用系统综合研究,采用解析方法将土地利用系统分解为自然子系统、经济子系统和社会子系统,对江苏省土地利用变化过程与格局进行分析。研究表明,耕地资源总量呈递减趋势,但粮食生产能力呈递增趋势,并表现出明显的地区分异规律;虽然经济总量也呈递增趋势,但信息熵指数表明区域分异明显;最后提出区域土地利用变化的“多层推—拉驱动”模型。  相似文献   

重力式码头CAD系统开发的荷载解决方案     

夏运强  陈兆林 《海岸工程》2006,25(1):6-14

针对重力式码头CAD系统开发中存在的设计荷载处理的技术难题,提出了一种切实可行的计算机解决方案,并提供了CAD系统常用的数据接口技术。该方案有较强的应用价值,可作为开发各类重力式码头CAD系统的借鉴。  相似文献   

Photogrammetric Reverse Engineering of the "Angel of the North"     

I. Newton  & J. P. Mills 《The Photogrammetric Record》1999,16(93):457-468

The Department of Geomatics and the Regional Centre for Innovation in Engineering Design in the University of Newcastle upon Tyne collaborated in a project to produce precise measurements for use in the fabrication of the body of the "Angel of the North" sculpture. This 20 m high edifice, by the sculptor Antony Gormley, is located adjacent to the A1(M) in Gateshead, Tyne and Wear.
This paper reviews the photogrammetric reverse engineering work carried out on a 1:10 scale plaster maquette of the "Angel of the North", which is a life-size model of the sculptor's body without any arms. The three dimensional measurements of the maquette, made by analytical photogrammetric techniques, were then processed to produce a fully functional three dimensional CAD model from which the dimensions needed by the fabricating company, Hartlepool Steel Fabrications Ltd., could be extracted. Additionally, the VirtuoZo digital photogrammetric software package was used to investigate the potential of automated measurement for this type of work and the results were compared with those obtained analytically.  相似文献   

渤海海峡及邻区现代小震震源机制解分析   总被引：2，自引：0，他引：2  

董旭光  周翠英  华爱军 《内陆地震》1999,13(1):7-16

以震源机制解资料推演并分析了渤海海峡及其周围地区现代构造应力场的总体特征、分区差异及地震破裂性质。认为构造应力场在某些局部与大区域之间有一定差异,而主张应力轴方位参数一致性稍好些,约在３３０°～３６０°之间,取向为北北西;构造应力场存在分区差异,尤以南北纵向差异明显;由于研究区内包含了地质构造和新构造活动性质各异的多个构造单元,地震破裂方向一致性较差  相似文献   

一维河流水质方程解析解性态的初步分析   总被引：1，自引：1，他引：0  

郭建青  李云峰 《水文》1999,33(6):30-33

采用较为简单的数学方法,建立了一维时投源河流水质方程解析解计算结果的统计参数与原始数据的统计参数间的近似关系,推导出描述该解析解计算问题性态的条件数,通过讨论,指明了计算问题属于“病态”和“良态”的条件。从而为正确使用该解析解解决实际水质问题提出了相应的建议。  相似文献   

基于除镉作用机理探讨的碳羟磷灰石溶解特性研究     

胥焕岩  王鹏  刘羽  彭明生 《矿物岩石》2005,25(4):6-10

碳羟磷灰石（CHap）在含镉溶液和空白溶液中溶解特性的对比实验结果表明：介质pH值是影响CHap溶解的重要因素,强酸务件下,溶解度最大;溶钙量和溶磷量的摩尔比均不是1、67;溶解初期阶段反应速度快,动力学过程复杂,后期阶段符合一级反应动力学特征,说明CHap溶解机理符合氢催化模型、非化学计量比溶解模型、多核模型,在含镉溶液中溶解时,还包括离子交换模型,即溶液中的镉离子与CHap中的钙离子发生交换作用。从溶解特性的角度推测：CHap除镉过程中存在有离子交换作用机理。  相似文献   

Relocation of the MS5.7 Earthquake Sequence in Songyuan, Jilin Province, 2018 and the Analysis of Its Seismogenic Structure     

An Yanru  Zhang Yingying  Yang Zhigao  Bai Lanshu  Liu Jie 《中国地震研究》2018,32(4):491-500

The 2018,Songyuan,Jilin M_S5. 7 earthquake occurred at the intersection of the FuyuZhaodong fault and the Second Songhua River fault. The moment magnitude of this earthquake is M_W5. 3,the centroid depth by the waveform fitting is 12 km,and it is a strike-slip type event. In this paper,with the seismic phase data provided by the China Earthquake Network, the double-difference location method is used to relocate the earthquake sequence,finally the relocation results of 60 earthquakes are obtained. The results show that the aftershock zone is about 4. 3km long and 3. 1km wide,which is distributed in the NE direction. The depth distribution of the seismic sequence is 9km-10 km. 1-2 days after the main shock,the aftershocks were scattered throughout the aftershock zone,and the largest aftershock occurred in the northeastern part of the aftershock zone. After 3-8 days,the aftershocks mainly occurred in the southwestern part of the aftershock zone. The profile distribution of the earthquake sequence shows that the fault plane dips to the southeast with the dip angle of about 75°. Combined with the regional tectonic setting,focal mechanism solution and intensity distribution,we conclude that the concealed fault of the Fuyu-Zhaodong fault is the seismogenic fault of the Songyuan M_S5. 7 earthquake. This paper also relocates the earthquake sequence of the previous magnitude 5. 0 earthquake in 2017. Combined with the results of the focal mechanism solution,we believe that the two earthquakes have the same seismogenic structure,and the earthquake sequence generally develops to the southwest. The historical seismic activity since 2009 shows that after the magnitude 5. 0 earthquake in 2017,the frequency and intensity of earthquakes in the earthquake zone are obviously enhanced,and attention should be paid to the development of seismic activity in the southwest direction of the earthquake zone.  相似文献   

山西运城Ms4.3、3.4两次地震波形特征和震源新参数对比分析     

梁永烨  王霞 《山西地震》2018,(1):7-9,31

对山西运城2016年3月12日Ms4.3和27日Ms3.4两次地震的波形特征和震源参数进行对比分析。结果显示,波形一致性很好,PmP波可能由于震源深度的差异,导致在同一台站的特征有所不同;震源机制解非常接近,说明两次地震的应力场作用方式一致。  相似文献   

基于震源机制解的鄂霍次克微板块东部俯冲带地区构造应力场反演     

王少坡  孙云强  解孟雨  魏东平 《中国地震》2020,36(2):181-199

基于国际地震中心(ISC)提供的1970年1月～2016年12月期间的地震震源机制解,对鄂霍次克微板块东部俯冲带地区进行了应力张量反演,得到了日本海沟、千岛海沟和勘察加海沟3个俯冲带区域的构造应力场特征。研究结果显示:①海沟地区浅部区域(h100km)的水平主压应力轴与西北太平洋板块的俯冲方位一致,与海沟走向近似垂直,其洋壳一侧以拉张型应力状态为主,而陆壳一侧则以挤压型应力为主,且在弧后区域均存在拉张的应力状态;80～200km深度范围区域表现出双地震带"Ⅰ"型构造应力场特征。②日本海沟带由于俯冲角相对较小(相比于千岛海沟和勘察加海沟),水平方向沿NWW向延伸更远,大洋板块与上覆板块之间耦合更加强烈,逆冲型地震发生数量最多。③对于深部区域(h300km),千岛地区应力场表现出非均匀性特征,可能是由地幔阻力导致的;而勘察加地区应力场表现出拉张型,可能是因为俯冲板片的拉伸拖曳作用更强。  相似文献