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对中国大陆1970年以来发生的1丛Ms≥7地震、7丛Ms≥6地震、2丛Ms5~6地震前的调制地震活动图像进行逐日时空扫描,发现强震丛前4级以上朔望调制地震的图像有一定的规律可寻。强震丛前,不同时段4级以上朔望调制地震会出现2种以上异常图像的相互转化,且强震丛开始前或活动期间,4级以上朔望调制地震和强震的走向有一定的一致性,这对预报地点有一定的指示意义。研究结果还显示,成丛强震前,同一时段在未来丛发地震的周围出现不同形式的4级以上朔望调制地震分布图像,表明同一时段出现不同形式和不同地域的调制地震异常分布图像后,可能会是一组强震的连发。研究结果表明,成丛强震前4级以上朔望调制地震的空间分布具有较好的中、短期前兆意义。 相似文献
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本文以中国大陆为具体研究对象 ,从大陆强震活动成组特征的客观性出发 ,开发了一种非线性动力学模型 ,用于模拟大陆强震成组活动特征及孕震环境对地震成组性的影响 ,运用此模型对一些地震活动特征和前兆场的演化特征进行了模拟和解释。地震活动的分布具有空间不均匀性和时间非平稳性。地震的空间不均匀性表现为地震在空间上往往成带、成区分布 ,地震的时间非平稳性表现为地震活动在时间轴上具有活跃和平静 (高潮和低潮 )相交替的特性。分析表明大陆地震具有明显的成组活动特征。强震活动的成组性是指强震活动在某些时段十分集中 ,呈成丛或丛… 相似文献
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本文把一个地区的地震活动看作泊松分布过程,分析了1965~1980年云南及邻近地区4级以上的地震活动,得出强震发生前,将出现中强震活动的密集时段和无震时段。这两个时间段的出现时间与未来强震的震级呈一定线性关系。本文的方法可供估计强震活动趋势参考。 相似文献
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该文基于1950年以来新疆周边强震与境内中强地震活动的统计分析结果, 解算了1976—2007年新疆周边强震活跃、 境内相对平静时段, 周边3组强震产生的库仑应力变化, 并结合其后3年新疆地区中强地震活动特征, 分析探讨了周边强震活动对境内地震活动的影响作用。 结果表明, 新疆周边这3组强震活动对新疆境内具有一定程度的减震作用。 相似文献
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根据阿部胜征新近研究和发表的均匀化全球大地震目录(1897——1980),获得如下几点关于全球强震活动性统计特征的初步认识:(1)本世纪六十年代中期之后,全球活动处于相对平静的阶段;(2)在全球活动高潮时段中b值偏低,大陆地震区的b值偏低;(3)据聚类分析方法研究序列的结果,全球不同的地震区内,存在几十年尺度的强震活动高潮幕和平静幕交替出现的现象;(4)北半球大陆浅源强震活动的空间分布和地球自转速率的变化特征有关。上述特征对估计全球和不同地震区的地震活动趋势可能有参考意义。 相似文献
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我国西北的甘、宁、青地区是强震活动十分突出的地区之一,历史上曾发生多次8级以上地震。但在1966—1976年我国大陆上一个地震活动高潮中该区却十分平静,预测在下一强震活动幕中西北地区可能成为强震的主体活动地区。北西向构造可能是强震发生的主要场所,强震发生于大震破裂区闭锁段上的可能性较大。1977年以来上述地区出现的中强地震活动增强和呈带分布已构成强震发生的背景异常,应密切注意该地区中小地震活动图象的变化。 相似文献
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本文改进了地震活动性模拟方法,使模型可以使用GPS反演得到的断层滑动速率的结果作为应力加载,进行区域的地震活动性模拟.选取太原地区作为研究区域,模拟并分析太原地区地震活动性.计算太原地区长达20000年的理论地震目录,通过对理论地震目录进行分析发现模拟结果的震级频度关系与实际观测资料具有相似性.太原地区的震级大于6级的模拟地震在时间上表现出很强的随机性,与年平均发生率为0.0129a~(-1)的Poisson过程对比,当采用卡方检验进行检验时,置信水平达到99.0%;然而,单一断层的强震的时间分布与相应年平均发生率的Poisson分布并不完全相近,部分断层拟合置信水平为90%左右,部分断层置信水平接近为0.这一结果表明,用Poisson过程估计太原地区长期地震发生率是比较合理的,估计单一断层上的地震危险性不是十分合理.地震危险性模拟结果显示,太原盆地地区7级以上地震的复现周期为4000年. 相似文献
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A. M. Korzhenkov J. R. Arrowsmith C. J. Crosby B. Guralnik E. A. Rogozhin A. A. Sorokin S. V. Abdieva A. B. Fortuna A. S. Yudakhin A. R. Agatova E. V. Deev J. V. Mazeika M. V. Rodkin J. Shen 《Izvestiya Physics of the Solid Earth》2018,54(2):252-268
The study and radiocarbon dating of the low alluvial terraces of the Chon-Aksuu River, in the Northern Issyk-Kul region, which were broken by the Kebin (Kemin) earthquake of 1911 (Ms = 8.2, Io = 10 to 11), are carried out. The obtained radiocarbon dated ages refer to the second half of the Holocene. Since that time, at least eight strong earthquakes took place along this (Chon-Aksuu) segment of the Aksuu border fault. Three seismic events, including the earthquake of 1911 occurred in the second millennium A.D. This outburst of seismic energy was preceded by two millennia of seismic quiescence, which set in after another pulse of seismic activation. The latter lasted for 1.5 millennia and included five strong earthquakes. The recurrence period of seismic events during the activations is 300–600 years. Hence, the seismic regime along the Chon–Aksuu segment of the Aksuu border fault in the second half of the Holocene was a succession of two seismic activations, each with a duration of 1.0–1.5 ka, which were separated by a 2-ka interval of seismic quiescence. Therefore, the absolute datings of the river terraces of different ages which have been broken by a seismogenic rupture can serve as a reliable source of information about the age of the strong earthquakes that occurred along the seismogenic fault. 相似文献
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Introduction The behavior of ground water is influenced by many factors, such as rainfall, exploitation ofground water, atmospheric pressure, tidal gravitation, ground stress variation, effect of surfacewater-body loads (or other loads) and other unknown factors. These factors change the dynamicstate of ground water to different extents and result in the diversification of ground water behavior.As for their mechanism, our knowledge is still superficial. Based on various images of water le… 相似文献
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In this article we have compared the results of seismotectonic and paleoseismogeologic investigations for representative segments
of the two fold systems of the Alpine-Himalayan mobile belt (in the North- west Caucasus and West Himalayas). It has been
found that during the previously identified “seismic gaps,” in both cases, we are dealing with primary dislocations (seismic
ruptures) of ancient historical and prehistoric strong earthquakes. According to estimations, the magnitude of one-act seismogenic
displacements in the first region was about 6.5-7.0 m, and the recurrence period ranges from 500 to 1500 years on average.
In the West Himalayas, the overthrust displacements along the ruptures were 6-7 m, which corresponds to an 8.0-magnitude earthquake.
At the same time, the recurrence period of strong earthquakes during a seismic gap in the Himalayas was 500-1000 years, which
is similar to that in the Caucasus. The data collected also demonstrate the correct preliminary estimation of the seismic
potential of zones of seismic quiescence in both the studied fold systems. 相似文献
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The conventional radiocarbon ages of soil horizons limiting the timing of six fault-generating dis- placements within the
East Sayan structure of the Main Sayan Fault and four displacements within the Tora structure of the Tunka Fault (M > 7) have
been calibrated according to the IntCal04 calibration curve. It was revealed that between time periods of 12 Ka and 5.4 Ka
years ago, the recurrence of earthquakes associated with movements along the faults in the East Sayan structure occurred once
every 3000 years. After seismic quiescence, since 1100 years, one earthquake has occurred every 440 years. Using the Monte
Carlo method, the possibility of the recurrence of strong earthquakes at different probability levels was considered. At a
fre- quency probability of 95% the Main Sayan fault may be hazardous, dating from about 2120 AD. When low- ering the threshold
probability to 72%, the beginning of the period of potential hazard is reduced to about 2030 AD. In both cases the maximum
possibility of the occurrence of the next strong earthquake is not earlier than in the 22nd century. For the Tora structure,
the periodicity of the recurrence of the earthquakes was esti- mated as 2800 yearsfor the past 11Ka with a probability of
over 95% of the recurrence of earthquakes. This allows us to assume that currently the Tora structure is within the time interval
of the potential risk of the recurrence of a strong earthquake. 相似文献
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本文应用1895年以来我国大陆地区7级和大于7级的强震资料,讨论了我国大陆强震活动的轮回特性,指出了我国大陆地区强震高潮的到来有一个发展过程,即经历强震活动的平静、增强及出现强震高潮三个幕。文中讨论了各幕的持续时间及其强震活动的频度和能量分布,同时还分析了各轮回中强震的地区分布,探讨了每个强震高潮的主体活动区的形成特点。这些结果可为研究我国大陆强震高潮到来和结束的标志及判断未来强震高潮的主体活动地区等强震预测问题提供线索。此外,本文还分析了我国大陆强震高潮与东北深震的相关关系等问题 相似文献