共查询到20条相似文献,搜索用时 784 毫秒
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通过对2009年7月9日姚安6.0级地震前的地震活动、前兆和宏观异常及其特征分析,认为前兆和宏观异常同步出现,对楚雄地区及邻区的中强地震有较好的对应关系。 相似文献
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作者于2013年6月底,前往芦山、雅安和成都等在“4·20”芦山地震中震感强烈的村镇,对地震前宏观异常信息开展了采集与调研.通过设计宏观异常调研问卷,与当地居民进行了一对一的访谈、共收集134份问卷,其中含有地震前宏观异常信息88条,包括动物、气象、地声、地磁、地下流体、地雾、人体7种类型.通过调研以及对调研问卷的分析表明,芦山地震前确实存在着一定数量和范围的宏观异常现象,芦山地震和汶川地震前宏观异常特征具有较大相似性.调研中还发现与城市相比,农村因动植物资源丰富,自然景观与自然现象相对少受人为干扰,是地震前宏观异常的主要发生地,因此,应该加强广大农村地区地震的认知培训和宏观异常上报信息平台建设,发挥专群结合在地震预测预报中的作用. 相似文献
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运用地下水、水文地质学、水力学、地震社会学、气象学等多方面的原理及观点,对非地震因素引起的吉林省地下水位及动物宏观异常从机理上进行剖析。同时提出了与强震前异常的主要区别。 相似文献
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Yao Daquan Shuo Zhi Shen Xiaoqi Chen Anguo Zheng Yingping Zheng Haigang Li Lingli 《中国地震研究》2010,24(3):363-370
During an excavation survey to the Daijiayuan vestige of the Western Zhou Dynasty-Late Spring and Autumn Period at Huoshan in Western Anhui,a ground crack related to tectonic movement and filled with silty fine sand was found. This phenomenon was initially confirmed to be due to seismic liquefaction. Many microscopic seismic relics,such as load structure,flow structure,cutoff plane and flotation of organic matter were found in the directional microscopic analysis of deformation. These discoveries and cognitions prove that there were two earthquake events taking place in the Western Zhou Dynasty-Late Spring and Autumn Period in this area. Above-mentioned works enrich and develop the research methods to identify prehistoric earthquake event in eastern China area to a certain extent. 相似文献
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利用分形方法对微观尺度下矿物微观组构及变化进行研究是目前的热点.本文以个旧芦塘坝矿段不同高度的硫化物矿石中广泛发育的黄铜矿为研究对象.建立起微观条件下的黄铜矿矿物的面积-周长(P-A)分形模型,并研究黄铜矿矿物的大小、不均匀性及空间分布特征.探讨黄铜矿这一标志性矿物在不同高度中的变化情况.结果显示随着深度从1758 m... 相似文献
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Yao Daquan 《中国地震研究》2005,19(1):35-42
1 RESEARCHINTOTHEACTIVITYTIMEOFFAULTSINBEDROCKAREASDatemeasurementoffaultactivityisessentialforrecognizingtheactivitybehaviorofafault,inversingseismologicalandgeologicaleventsandprobingintoearthquakerhythms .Itismoredifficulttodeterminetheactivitytimeoffa… 相似文献
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Anna Gotkowska‐Płachta Zofia Filipkowska Ewa Korzeniewska Wojciech Janczukowicz Beverly Dixon Iwona Gołaś Damian Szwalgin 《洁净——土壤、空气、水》2013,41(5):429-436
Experiments were conducted to study the airborne microbial contamination generated by a wastewater treatment plant (WWTP). Aerosol samples were collected simultaneously, by sedimentation and impact methods, from the area and the surroundings of the WWTP. Total colony forming units (CFUs) of heterotrophic bacteria (HPC), as well as members of the Enterobacteriaceae, staphylococci, enterococci, actinomycetes, and microscopic fungi were determined. Bacterial (HPC) concentrations ranged between 101 and 104 CFU/m3, fungi 0 and 104 CFU/m3. Higher numbers of HPC bacteria in air samples were observed in summer, fungi in autumn. The main emission of microorganisms to atmospheric air was from the mechanical sewage treatment devices of the WWTP. The facilities of the biological sewage treatment of the plant did not generate large amounts of bioaerosols. In the air obtained from the premises of the WWTP, 25 species of the Enterobacteriaceae were isolated (Salmonella spp., Klebsiella pneumoniae, Escherichia coli). At the fence and in the surroundings only Pantoea spp. were identified. This suggests that the sewage bacteria were mainly discharged in the area of the WWTP. The presence of enteric bacteria, especially Enterobacteriaceae reflects the level of air pollution with bioaerosols from sewage and is an important factor during monitoring the quality of the air around WWTPs. 相似文献
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断裂微观滑移方式标志在地震安全性评价中的应用 总被引:1,自引:0,他引:1
将笔者近年来总结归纳出的活动断裂滑动特性民引入重大工程场地地震安全性评价工作中,结合样品的产出环境及宏观和超微观滑移特性标志分析,对样品所反映的最新活动方式进行鉴定,并在实践中补充和完善识别标志,从而为工程场地地震环境分析提供微观依据。 相似文献
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本文基于Biot理论,考虑了多孔介质中固体骨架的松弛特征,引入了纵波品质因子、横波品质因子与耗散品质因子三参数来描述黏弹双相介质波动方程.采用虚谱法在地震频段进行了波场模拟,模拟结果表明:松弛骨架机制不仅适用于高频段,也可用于解释地震频段下的弹性波衰减现象,以描述固体微细颗粒的中观松弛特征.结合小生境遗传算法对三层模型24个介质参数进行了反演,反演结果表明:无噪波场的反演结果具有较高精度,对于含噪波场,取值在奇异点附近的介质参数反演精度降低.最后,对中国东部某地区的实际资料进行了浅层参数的反演,得到了该地区的表层固体体积模量、固体密度以及品质因子. 相似文献
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岩石的脆性-延性转变及塑性流动网络 总被引:12,自引:0,他引:12
实验变形研究表明.随着矿物组成.粒度、温度、围压、应变率、液体介质等因素的变化岩石由脆性,半脆性,向半延性.延性转变,其中包括力学行为.微观机制和宏观结构的变化,而决定岩石脆性-延性转变的基本因素在于所含的粘塑性成分及其粘滞性.半延性流动具有共轭网络状的结构特征;延性流动则包括网络状流动和均匀流动两种宏观结构;半延性-延性流动网络以其近似正交性和非牛顿流动特性分别与半脆性破裂网络和均匀延性流动相区别.基于上述研究,可将地壳、上地幔划分为脆性-半脆性的中上地壳,半延性-延性网络状流动的岩石圈下层(含下地壳和岩石圈地幔)和均匀延性流动的软流圈.地壳多震层内的大型地震带及网络是岩石圈下层塑性流动网络的一种响应. 相似文献