应用神经网络建立加速度峰值衰减规律   总被引：2，自引：0，他引：2  

崔建文  温瑞智 《地震研究》1997,20(3):278-285

在假定了加速度峰值衰减规律的形式后，本采用人工神经网络拟合实际加速度峰值观测资料来求取方程中的待定系数。为加速神经网络的训练，本设计了基于ＢＰ学习算法的目标分段网络训练法。  相似文献   

构造机理与地震大形势分析     

夏玉胜  胡爱真  唐燕红 《高原地震》1997,(4)

对全球大震时空特征的分析表明，北南半球大震分布与陆地面积成比例，全球强震活动具有35年的地极移周期，并对一些具有全球活动特征的构造事件进行了机理探讨，最后对大陆西部强震的活动规律．尤其是主体活动区的特点进点了仔细的研究。给出了未来一段时间内的预测结果。  相似文献   

云南地区1995～1996年三次强震爆发的共性研究     

赵洪声 《华南地震》1997,17(1):34-38

论述了在１９９５～１９９６年云南地区发生的孟连西南７．３级，武定６．５级和丽江７．０级３次强烈地震的孕育过程中，近源区中小地震的异常增频特点和临震前大气压力的突变共性，并据此提出，强震的发生乃是地壳内外力涨落地加剧的结果。  相似文献   

湖南省黄石水库诱发地震的形成条件及成因探讨   总被引：2，自引：0，他引：2  

戴宗明 《四川地震》1997,(4):58-63

在湖南桃源县黄石水库库区，由于张扭性活断层和深部岩溶的存在，水库蓄水后产生的附加应力场及水库区增强的岩石孔隙流体压力诱发了断层的断滑，使得库区应力集中区和岩溶发育区合二为一的地带发生构造型地震，从而在震活动的时间序列、空间规律，地震与库水位关系，震源深度、震情等方面表现出构造水库诱发地震的特点。  相似文献   

湖南东江水库诱发地震   总被引：1，自引：0，他引：1       下载免费PDF全文

胡平  陈献程 《地球物理学报》1997,40(1):66-77

东江水库自蓄水前约半年起就开始进行地震监测，发震后通过密集台网强化观测、震源机制解及地震地质等多项工作，综合研究该库诱发地震发震原因，认为由于库水渗透引起的多种局部性应力调整导致水库诱发地震活动．其发展趋势将表现为逐渐衰减，今后不致于发生破坏性地震．  相似文献   

华北地区大震前区域地震活动的中短期变化          下载免费PDF全文

林怀存  刘希强 《地震地质》1997,19(1):38-42

对发生在华北地区３１个Ｍ≥５地震震前区域地震活动的时间序列进行的研究得出：（１）华北地区发生Ｍ≥５地震前，区域地震活动的短期平静现象与大震发生的相关性很强。３１个Ｍ≥５地震前的平静时间主要集中在２０～８７ｄ，１２０～２１０ｄ和大于２１０ｄ。同时还得出大震前的短期平静时间与震级大小无关的结论；（２）区域地震活动在短时间内出现增强趋势，与发生大震的相关性很弱，相关的仅占总数的６．４％  相似文献   

An estimate of hypocentre location accuracy in a large network: possible implications for tectonic studies in Italy     

Rita Di Giovambattista  Salvatore Barba 《Geophysical Journal International》1997,129(1):124-132

Data recorded by the Italian Telemetered Seismic Network (ITSN) of the Istituto Nazionale di Geofisica (ING) have been widely used in recent years to image slab structures and to find evidence for active processes along the Italian Peninsula. However, the use of seismic data for geostructural purposes may be affected by the well-known trade-off between earthquake location and seismic-velocity parameters. Furthermore, the confidence ellipse predicted by standard procedures may be inadequate for the representation of the probable error of a computed localization. This paper evaluates the probable errors on the hypocentre determinations of the seismic events recorded by the ITSN, using a Monte Carlo method.
We compute synthetic arrival times using a 1-D velocity model appropriate as an average for the Italian area. The hypocentres used are all those recorded by the ITSN during the period January 1992 to March 1994 (1972 events). Station locations are those of the current ITSN configuration. The synthetic arrival times are perturbed with a Gaussian distribution of errors and input to ING's standard hypocentral location procedure, but using crustal velocities differing by 10 per cent from those used to generate them. Each simulation is repeated at least 30 times. Average absolute shifts of hypocentres are assessed in grid cells of linear dimension 33 km covering the whole Italian region.
For regions within the ITSN, shifts are typically 5–10 km in location and up to 20 km in depth. However, for offshore and coastal regions, they are much greater: 50 km or more in both location and depth (far exceeding the equivalent uncertainties quoted by ING bulletins). Possible consequences of this are highlighted by producing a cross-section of subcrustal hypocentres from the Adriatic to the Tyrrhenian Sea, where the large uncertainty in depth precludes any confident interpretation of dipping tectonic features.  相似文献   

Seismicity re-evaluation of the northern Red Sea     

A. Gharib  A. Necioglu  A. Al-Amri 《Geophysical Journal International》1997,130(2):335-348

The Aqaba subnetwork of five vertical short-period stations of the seismological observatory of King Saud University was installed in late 1986 along the eastern side of the Gulf of Aqaba, northern Red Sea. During the first six years (1986 August to 1992 July) of the subnetwork operation, 400 microearthquakes were detected. Of these, 93 events were recorded by most of the subnet stations and were located. Their epicentres lie in the northern part of the Red Sea between latitudes 25.5 N and 27.5 N and longitudes 33.5 E and 36 E along the axial depression of the Red Sea where the large intrusions (deeps) are located. Magnitudes of the locatable events ranged from 2.1 to 4.8. Two intensive swarms of about 200 microearthquakes occurred in February and June of 1992. The February swarm is the first intensive sequence observed in the surveying area since the establishment of the KSU network. Frequency-magnitude analysis of the recorded events for the period 1986-1992 yielded 3.543 for a and 0.658 for b . These relatively higher b values (0.658) are a good indication of the crustal heterogeneity under the spreading zone of the northern Red Sea. USGS and KSU data together show 3.41 for a and 0.49 for b . This study, together with historical data, confirms that the area is very seismically active and that the activity is mainly of swarm type, and may be attributed to the subsurface magmatic activity and spreading centres that are usually associated with strike-slip and normal faulting, respectively.  相似文献   

Three-dimensional velocity structure of the upper mantle beneath Costa Rica from a teleseismic tomography study     

D. Colombo  G. B. Cimini  R. de  Franco 《Geophysical Journal International》1997,131(2):189-208

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Inelastic models of lithospheric stress-11. Implications for outer-rise seismicity and dynamics     

Steve Mueller  William Spence  George L. Choy 《Geophysical Journal International》1996,125(1):54-72

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