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1.
Yufen Gao 《地震学报(英文版)》1992,5(1):127-131
The geomagnetic daily variations of vertical component, which were recorded by geomagnetic array in Jiangsu Province, are
investigated with the method of multichannel Wiener filtering. The results show that the daily standard errors between raw
data and the actual output of the filter for the nearest stations away from epicenter are obviously higher than ordinary level
before the Huanghai earthquake, especially three days before, then returned to normal after the earthquake.
The Chinese version of this paper appeared in the Chinese edition ofActa Seismologica Sinica,13, 76–79, 1991.
The project was supported by the Chinese Joint Seismological Science Foundation. 相似文献
2.
A three-component geomagnetic survey was carried out during the period from 2002 to 2004 in China including Jiujiang-Ruichang region. Comparing the ＂2005.0 surface spline model of China geomagnetic field＂ created on the basis of the survey data with the ＂1970.0 surface spline model of China geomagnetic field＂, we can see an obvious abnormity in the geomagnetic horizontal component within a range of about 100 km around the epicenter of the Ms=5.7 Jiujiang-Ruichang earthquake occurred on November 26, 2005. After the earthquake, we carded out a repeated geomagnetic survey at 21 stations in the Jiujiang-Ruichang region and created a corresponding ＂2005.0 partially revised surface spline model of China geomagnetic field＂. By comparing the above three models, analyzing the geomagnetic horizontal component at the profile in the Jiujiang-Ruichang region and quantitatively studying the geomagnetic data of every stations around the Ms=5.7 earthquake, we have obtained the geomagnetic abnormity associated with this earthquake. Then the geomagnetic abnormity and its relation with seismic activity are discussed in this paper. 相似文献
3.
Using observational data of geomagnetic total intensity from 13 stations in the Beijing-Tianjin region, 3 stations in the
western Yunnan region of China, and 6 stations in California of U. S. A., the daily variations and their spectra of geomagnetic
total intensity were analyzed and compared. The results show that the morphology, the range and spectrum of daily variations
in geomagnetic total intensity are basically the same within the local extent of 100–200 km and are different in the large
extent of 500 km. The latitude factor of the daily variation range of geomagnetic total intensity is about 1–2 nT/degree within
the latitude extent of 25°–40°.
The Chinese version of this paper appeared in the Chinese edition ofActa Seismologica Sinica,14, 83–89, 1992.
This work is supported by the State Seismological Bureau and the Chinese Joint Seismological Science Foundation, and U.S.
Geological Survey. 相似文献
4.
Ren Xi-xian 《地震学报(英文版)》2006,19(1):87-92
A new concept is suggested on tectonomagnetic research about the noise in simultaneous geomagnetic difference data caused
by the effect of S
q local-time variation, together with the method of theoretical calculation. The level of the noise and its contribution to
the total noises of the differences data are analyzed. The result indicates that the noise increases linearly with the increase
of the distance between the two stations in the range of 40° longitude-difference, and its increasing rate is about 0.4 nT/(°)
at latitude 40°N. The example calculated at a pair of sites with longitude-difference 0.357°, shows that the noise is about
one fifth of the total noises of the difference data on geomagnetic quiet-day.
Contribution No. 06FE3008, Institute of Geophysics, China Earthquake Administration. 相似文献
5.
Since 1979 the repeated observations and experiments of geomagnetic total intensity and vertical component have been carried
out for ten years in the geomagetic network which is located in Jiangsu Province, China. Three earthquakes aboveM
s 5.0 occurred during the decade, and some seismomagnetic effects were observed. The observation results show that the anomalies
of the vertical geomagnetic component can’t be observed untill some months before the earthquake (M
s>5.0) in this area.
In this paper it is suggested that a densely distributed network for continuous observation of geomagnetic vertical component
may catch seismomagnetic anomalies and thus improve earthquake prediction in the light of the geomagnetic measurements of
the mid — or — low latitude locations.
The Chinese version of this paper appeared in the Chinese edition ofActa Seismologica Sinica,13, 80–87, 1991.
This study is sponsored by the Chinese Joint Seismological Science Foundation. 相似文献
6.
运用地磁加卸载响应比方法(LURR)对华北地区23个地磁台站2008—2014年的数字化地磁相对记录数据进行计算分析,结果显示华北地区7年内发生了38次共计10组加卸载响应比异常,其中7组有震例对应,在选定的24次震例中16次有震前异常。经统计发现各次异常发生时其异常面积与最大异常强度成正比关系,各组异常内累计异常台站数量与组内地震辐射能量有一定相关性。对有震例的7组异常分析后认为多数情况下组内各次异常之间有一定联系,主要表现为位置的连续性及继承性,并且发现震中位置和异常位置分布有一定关系。 相似文献
7.
Time changes in transfer functions of short period geomagnetic variations in 28 years from 1960 through 1987 are studied,
systemically and in detail in this paper. The results indicate that: (1) It is evident that seasonal and secular changes in
the transfer functionsA at exist the Guangzhou Geomagnetic observatory. The characteristics for seasonal changes are large in summer and smaller
in winter with main cycles of 12 and 6 months. The characteristic for secular change is a descend with a rate of 0.0025 per
year. The seasonal and secular changes in transfer functionsB are not evident. (2) The direction of Parkinson vector at Guangzhou geomagnetic observatory is clearly affected by the ocean,
and is associated with coastal effect. (3) The values of the transfer function A and B are related to geomagnetic activity
ata=0.05. Secular change is not related to geomagnetic activity, maybe it is affected in a great measure by earth conductivity
change.
The Chinese version of this paper appeared in the Chinese edition ofActa Seismologica sinica,13, 480–488, 1991.
This study is part supported by Chinese Joint Seismological Science Fundation. 相似文献
8.
ＩｎｔｒｏｄｕｃｔｉｏｎＩｔｉｓｋｎｏｗｎｔｈａｔｔｈｅｅｌｅｃｔｒｏｍａｇｎｅｔｉｃｉｍｐｅｄａｎｃｅｓｏｆｔｈｅｃｒｕｓｔｍｅｄｉｕｍｍａｙｂｅｃｈａｎｇｅｄｄｕｒｉｎｇｔｈｅｐｒｅｇｎａｎｃｙｏｆａｎｅａｒｔｈｑｕａｋｅ,ａｎｄｍａｙｌｅａｄｔ... 相似文献
9.
This paper has made a study of the relationship between the phases of seismic activities from 1966 to 1976 in the region of
the North China Block and the temporal and spatial evolution of temperature anomalies from February 1960 to January 1979 of
the greater North China. The main conclusions are: (1) The temperature variation from February 1960 (rise) to January 1977
(drop) and the temperature rises of September 1975 and February 1976 are connected with the beginning and conclusion of phases
of seismic activity. (2) The relation between the time-duration and the extent of temperature anomaly and that between these
two parameters and the energy released by an earthquake have high credibility. (3) If the time period of 16.5 years between
February 1960 and July 28, 1976, the occurrence time of the the great Tangshan earthquake, is divided into 18 time intervals
according to 0.618N, the earthquakes in this phase of seismic activity and temperature rises fall just into the same intervals.
The Chinese version of this paper appeared in the Chinese edition ofActa Seismologica Sinica,15, 76–82, 1993. 相似文献
10.
Temperature is an important factor affecting seismic velocity, and terrestrial heat flow is the most direct indication of
temperature distribution of the lithosphere. Some authors therefore suggested that Pn velocity should be inversely related
with heat flow. The average heat flow values (q) and Pn velocities (V
Pn) in 22 areas have been calculated and collected from published literatures to investigate the possible correlation between
these two parameters for the continental area of China. However, the results show that the variations ofq andV
Pn in the studied areas are far away from the expected inverse relation. The effects of pressure of seismic velocity and contribution
of crustal radiogenic heat on heat flow have been taken into consideration in regressions respectively and simultaneously.
However, all the corrections are of little help for the improvement of the expected inverse relation. The conclusion deduced
from the present study is that in a large scale region with complex tectonic evolution history and complex deep structure
framework such as the continental area of China, temperature at the Moho boundary is not the most important factor affecting
Pn velocity. The conceptual inverse correlation between heat flow and Pn velocity might be masked by various “noises”.
The Chinese version of this paper appeared in the Chinese edition ofActa Seismologica Sinica,14, 42–50, 1992. 相似文献
11.
In this paper, by means of the statistical analysis method of stochastic spatial point process, statistical analysis of spatial
distribution of earthquakes in the large northern region of China is made. Emphasis is on the test and analysis of the complete
spatial randomness, correlation of earthquake distribution in the different magnitude interval and random labeling. It is
shown by the analysis that the spatial distribution of earthquakes in the large northern region is “clustered”, the distributions
of earthquakes in different magnitude interval are positively correlated and can be modeled by a two-dimensional process.
The results obtained in the paper can be used for the establishment of a reasonable spatial distribution model and have some
application in the reasonable estimation of seismic hazard.
The Chinese version of this paper appeared in the Chinese edition ofActa Seismologica Sinica,15, 129–135, 1993. 相似文献
12.
To actually reflect the seismic temporal-spatial inhomogeneity of intra continental strong earthquakes of North China in seismic
hazard analysis, several seismological and geological characteristics have been selected and quantized to describe the seismicity
features in time and space of every magnitude interval with the thought of dividing the interesting magnitude range into several
intervals and using of spatial probability distribution function. A component analysis method with orthogonal transformation
is introduced to avoid the repeated use of the same element and the subjective effects in determining the annual earthquake
occurrence rates of earthquake. By passing synthetic fuzzy judgement on the nonintercorrelated new characteristics, the annual
occurrence rates of every magnitude interval of each potential source area are obtained associated with the adjustments of
earthquake reducing process after the occurrence ofM>7 quake. An intensity map of the Beijing-Tianjin-Zhangjiakou area is calculated as an example which shows a close coincidence
with the seismic temporal-spatial inhomogeneity of North China.
The Chinese version of this paper appeared in the Chinese edition ofActa Seismologica Sinica,13, 496–504, 1991. 相似文献
13.
14.
Tectonic forces from the relative movements between plates are transmitted into the continental crust, and then they create
the earthquake generating stress field there. The space-time distribution of the seismic activity including the small earthquakes
in a region reflects the variation of the stress field in the region.
According to this idea, the characteristics of the stress fields in the various regions of East Asia have been analyzed in
detail in this paper based on a lot of solutions of focal mechanisms and data of seismic activity during the last 500 years.
The results indicate that the tectonic forces from the subduction of the Pacific Ocean plate underneath the Eurasian plate
control the stress field in the region from North China to the northern part of the North-South Seismic Belt.
The variation of the regional stress field shown by the variation of seismic activity in some regions of Japan has also been
discussed based on characteristics of variation of the seimicity of small earthquakes.
Synchronous variations of seismicity in the past 100 years or so in West China and in the boundary region between the Indo-Australian
and Eurasian plates implicate that there is the transmission of tectonic forces into West China through the collision between
the Indo-Australian and Eurasian plates. The active seismic activity in the boundary region between the Indo-Australian and
the Eurasian plates and in West China is continuing consistently.
The Chinese version of this paper appeared in the Chinese edition ofActa Seismologica Sinica,13, 287–294, 1991. 相似文献
15.
The intterrelation among strong earthquakes and its application are emphatically studied in this paper. Taking North China
seismic region as study area, we have investigated how a great earthquake influence other strong earthqukaes in neighbouring
area? Does there exist earthqukae immunity phenomenon? If it exists, what distributional pattern did it has in space-time
domain? The results show that occurrence of earthquakes withM⩾7 has cetain immunity phenomenon to earthquakes withM⩾6 in North China. Among others, the immunity area of earthquakes withM=8 is much larger than that ofM=7. For earthquakes withM⩾8, the immunity area to the earthquakes ofM=7 is larger than toM=6.
Based on the above analysis, using some statistical methods, we gave the variational regularity of seismic immunity factor
with space and time, and explored its concrete application in seismic hazard analysis.
The Chinese version of this paper appeared in the Chinese edition ofActa Seismologica Sinica,15, 339–346, 1993. 相似文献
16.
In this paper, the two metnods, rectangular spectrum (RS) and maximum entropy power spectrum (MES), have been used in calculating
the geomagnetic structures of the crust in Haicheng and its adjacent areas and carrying out the geomagnetic stratification
of the crust. The result of the research indicates that the crust can be devided into such three layers as nonmagnetic layer,
magnetic layer and regressive magnetic layer from the top to the bottom. It is also found the distribution of the geomagnetic
bottom interface (Curie surface) is consistent with the lower interface of the upper crust and the top interface of the middle
crust of the velocity structure of the crust. It is very interesting that the Haicheng earthquake of Feb. 4, 1975,M 7.3 occurred at the depth gradient belt of the Curie isotherm surface. So, to research on the geomagnetic layers and the
distribution characteristics of the Curie isotherm surface is meaningful in judging potential seismic foci.
The Chinese version of this paper appeared in the Chinese edition ofActa Seismologica Sinica,15, 448–454, 1993.
The data of velocity and electricity materials used in this paper are as reference from the related materials of the maps
and directions etc. of Donggou-Haicheng-Dong Ujimqin Qi Geoscience Transect by Prof. Zao-Xun LU, Huai-Kuan XIA and others. 相似文献
17.
2010年1月11-24日,华北地区出现7次地磁低点位移异常。异常结束1天后研究区内发生2010年1月24日山西河津4.8级地震。采用实测低点时间减去理论低点时间的方法剔除低点时间经度效应,并以剔除经度效应后低点时间为0 h的等值线作为低点位移分界线,山西河津4.8级地震震中处于1月16日、17日、19日、22日地磁低点位移分界线上。低点位移异常日期间,华北地区存在显著的高梯度带,该文采用梯度值定量描述低点时间空间变化程度。在正常日期间,华北地区未出现梯度值大于1 h/（°）的区域,在异常日期间,出现梯度值大于1 h/（°）的区域,河津4.8级地震多位于高梯度区边缘。 相似文献
18.
According to geological tectonics and seismic activites this paper devided North China (30°–45°N, 105°–130°E) into four areas.
We analyzed the North China earthquake catalogue from 1970 to 1986 (from 1965 to 1986 for Huabei, the North China, plain region)
and identified forty-two bursts of aftershock. Seven of them occurred in aftershock regions of strong earthquakes and seventeen
of them in the seismic swarm regions. The relation between strong earthquakes with the remaining eighteen bursts of aftershocks
has been studied and tested statistically in this paper. The result of statistical testing show that the random probabilityp of coincidence of bursts of aftershock with subsequent strong earthquakes is less than six percent. By Xu’sR scoring method the efficacy of predicting strong earthquake from bursts of aftershock is estimated greater than 39 percent.
Following the method proposed in the paper we analyzed the earthquake catalogue of China from 1987 to June, 1988. The results
show that there was only one burst of aftershock occurred on Jan. 6, 1988 withM=3.6 in Xiuyan of Northeast China. It implicates that a potential earthquake withM
S⩽5 might occur in one year afterwards in the region of Northeast China. Actually on Feb. 25, 1988 an earthquake withM
S=5.3 occurred in Zhangwu of Northeast China. Another example is Datong-Yanggao shock on October 18, 1989 which is a burst
of aftershock. Three hours after an expected shock withM =6.1 took place in the same area. Two examples above have been tested in practical prediction and this shows that bursts
of aftershocks are significant in predicting strong earthquakes.
The Chinese version of this paper appeared in the Chinese edition ofActa Seismologica Sinica,13, 273–280, 1991.
Part of earthquake catalogue is from Jinbiao Chen, Peiyan Chen and Quanlin Li. 相似文献
19.
This paper systematically summarized the relation of the abnormal change of He and H2 dissolved gasses in deep hot-water well at Beijing No. 2 Cotton Mill and their relation with seismicity of the region. An
empirical formula for the relation of the precursory anomaly of He and H2 gasses with the magnitude and occurrence time of earthquake has been derived. Two events of magnitude greater than 5 in North
China had been successfully predicted by using this formula.
The Chinese version of this paper appeared in the Chinese edition ofActa Seismologica Sinica,15, 490–497, 1993. 相似文献
20.
Based on 141 data of in-situ stress orientations data of breakouts, stress reliefs and hydraulic fracture tests, and some
data of stress magnitudes from oil-well hydrofracturing operations, this paper discusses in-situ stress regime and the tectonic
stress provinces in the China’s Sea and adjacent areas. Furthermore, the origin of tectonic stress field is expounded.
The research results show that the tectonic stress in China’s Sea region can be divided into some stress provinces which are
the extension of the Northern China and Southern China stress provinces toward the eastern sea area. The tectonic stress field
in the Bohai and Huanghai and their neighbouring regions is controlled by a ENE-WSW compression, where the faulting types
are mainly strike-slip. However, the stress in the East and South China’s sea region and the Taiwan Straits is dominated by
the WNW-NW-NNW compressions, that is to say that the orientations of the maximum horizontal stress spread radially from the
central mainland toward southeastern sea areas. The principal stress directions become more and more steady and uniform as
depth increases. In the North China and nearby areas, the types of faulting are primarily strike-slip. In Southern China and
adjacent sea areas, there is a transition layer at 1,700M depth, the faultings principally show reverse faults above that
depth and strike-slip below it. Furthermore the origin of the tectonic stress field in this region may primarily come from
the composite action of the Pacific, the Philippine sea and the India-Australian plates.
The Chinese version of this paper appeared in the Chinese edition ofActa Seismologica Sinica,14, 17–28, 1992. 相似文献