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901.
研究了1500年以来东南沿海地震区东部中强地震的活动特征。通过对其时序演变进程的分析,长乐-诏安地震带和邵武-河源地震带地震活动参数的对比,以及对第二活跃期中强地震迁移特点的研究,对该区今后的地震活动趋势作出了估计。 相似文献
902.
本文采用多分形的方法研究了四川西部地区20年来的地震活动的空间分布特征.对D_q谱与D_(-1),D_(-2)曲线结合震例进行分析,指出其变化与强震活动有密切联系。并结合空区理论,认为D_q(q<0)主要描述了地震空区的情况,该方法在地震前兆信息提取有中重要意义。 相似文献
903.
震前大气电场异常的区域性特征 总被引:4,自引:1,他引:4
在了近场每次较大地震发生前,均能观测到明显的大气电场负异常信息。在观测不到明显的大气电场负异常时,近场近期一般不会有较大地震发生的基础上,本文对北京及其附近地区为例,利用所观测到的在气电场异常资料及1985年后该地区所发生的8次Ml≥4地震资料,较深入地探讨了震前大气电场异常的空间分布特征,取得了一些规律性的认识:(1)异常多发生在距震中不太范围内,且随着震级的增大异常区的范围也增大。(2)较大地 相似文献
904.
刘明生 《地震地磁观测与研究》1993,(5)
介绍了一种适用于遥测地震台网台站钟控脉冲标定的IC-D新型脉冲标定电路. 相似文献
905.
906.
907.
Xue-Ze Wen 《地震学报(英文版)》1993,6(4):993-1004
Spatial distribution of sources of strong and large earthquakes on the Xiaojiang fault zone in eastern Yunnan is studied according
to historical earthquake data. 7 segments of relatively independent sources or basic units of rupture along the fault zone
have been identified preliminarily. On every segment, time intervals between main historical earthquakes are generally characterized
by “time-predictable” recurrence behavior with indetermination. A statistic model for the time intervals between earthquakes
of the fault zone has been preliminarily established. And a mathematical method has been introduced into this paper to reckon
average recurrence interval between earthquakes under the condition of having known the size of the last event at a specific
segment. Based on these, ranges of the average recurrence intervals given confidence have been estimated for events of various
sizes on the fault zone. Further, the author puts forward a real-time probabilistic model that is suitable to analyze seismic
potential for individual segments along a fault zone on which earthquake recurrence intervals have been characterized by quasi-time-predictable
behavior, and applies this model to calculate conditional probabilities and probability gains of earthquake recurring on the
individual segments of the Xiaojiang fault zone during the period from 1991 to 2005. As a consequence, it has shown that two
parts of this fault zone, from south of Dongchuan to Songming and from Chengjiang to Huaning, have relatively high likelihoods
for strong or large earthquake recurring in the future.
The Chinese version of this paper appeared in the Chinese edition ofActa Seismologica Sinica,15, 322–330, 1993. 相似文献
908.
Meng-Tan Gao 《地震学报(英文版)》1993,6(3):713-719
The models currently used in the seismic evaluation of important projects, microzoning and seismic zonation are all for site.
Although seismic hazard analysis have been done for many sites in seismic zonation and microzoning, relationship among sites
is not considered in the final results. Studies show that it is impossible to get total hazard for specific area from the
results of the hazard analysis of sites. So, when we consider the total seismic hazard of a specific spatial distributed system,
methods for site are not enough. Author discussed the relation and the difference between system hazard and segments hazard
which form the system and proposed a seismic hazard analysis model taking spatial linear distributed series and parallel system
as an example. In aseismic design and earthquake disaster prevention decision, not only the seismic hazard of segments of
the system but also the total seismic hazard of the system should be considered.
The Chinese version of this paper appeared in the Chinese edition ofActa Seismologica Sinica,15, 347–352, 1993. 相似文献
909.
Moment tensors of eleven major earthquakes in the Tibetan Plateau and its surrounding region from 1966 to 1980 are estimated
by generalized inverse technique. The seismic source time function and focal depth are immediately determined in the inversion.
The results show that moment tensors of some events differ significantly from double couple, the deviation increases with
decreasing plunge angle of null axis. All these events occurred in the upper crust, much shallower than those reported so
far, for example, in NEIS Bulletin. Focal mechanism solution obtained from the moment tensors are consistent with the idea
that the Indian plate collides northwards with the Eurasian plate and that an eastward spreading exists in the crust of the
Tibetan Plateau. The stress drops for earthquakes of intraplate are systematically higher than those of earthquakes in suture
zone. The source process duration becomes longer with seismic moment, but for the same seismic moment, the process duration
for earthquakes in suture zone is about 1.4 times of those for intraplate event, these results suggest that the earthquakes
near suture zone may be of a special characteristics in source process differently from those in intraplate.
The Chinese version of this paper appeared in the Chinese edition ofActa Seismologica Sinica,14, 423 – 434, 1992. 相似文献
910.
We have employed 10 digital records and computed the spectral magnitude and the seismic radiated energy for 18 large earthquakes
(M
s≥6) occurred in Eur-asian belt during 1986–1989. The nine digital stations (CD-SN) distribute all over China and one in Germany.
The spectral magnitudes of various period have different stability among stations. The stability is better for maximum spectral
magnitudemi and seismic radiated energyE, their differences among stations are smaller, especially for the stations where the ray path main penetrates the low mantle.
But the stability of corner period is usually not good. The relation between seismic radiated energy and seismic moment magnitudeM
w is lg (E)=1.5Mw+c, wherec is a constant. The maximum spectral magnitudemi=M
w+0.1, it is consistant with theoretical prediction.
The Chinese version of this paper appeared in the Chinese edition ofActa Seismologica Sinica,15, 418–426, 1993.
This work supported by the Deutsche Forschungsgemeinschaft, Bonn, F. R. Germany. The support is grateful acknowledge. 相似文献