根据历史地震资料分析渤海中部与胶辽海峡地震周期模式。
Earthquake recurrence model in middle Bohai Sea and Jiaoliao Haixia is analyzed based on history earthquake data.
震后趋势早期判定在一定程度上依赖于历史地震的震型经验。
Early estimating trend after earthquake depends on the experience of types of historical earthquake sequence in some extent.
最后，对今后“安评”工作中的历史地震目录的使用提出建议。
Then some suggestions are put forward on the use of historical earthquake catalog.
论述了山西应县木塔在历史地震和工程抗震研究中的地位和意义。
Significance and importance of Yingxian Wooden Tower of Shanxi in historical earthquake and antiseismic engineering research are discussed.
根据历史地震资料，分析了渤海中部与胶辽海峡的地震周期模式。
The earthquake period model in middle Bohai Sea and Jiaoliao channel is analyzed based on history earthquake data.
在地震危险性分析中，历史地震资料是确定地震活动性参数的关键。
The historical seismic data are the key determining seismicity parameter in seismic hazard analysis.
地震伤亡人数超过1992年，也高于历史地震灾害的平均死亡人数。
The earthquake casualties exceeded that of 1992, and were also higher than the annual average of historical earthquake casual-ties.
编制完整可靠的历史地震目录是地震安全性评价工作的一项基础工作。
But there are some arguments on some earthquake parameters in the new version "historical earthquake catalog in China a."
史料记载表明安徽地区历史地震以中强震为主，最高震级为M614级。
Historical earthquake records show that most historical earthquakes in Anhui area are medium-strong earthquakes, the largest magnitude of them is M614.
近年来，在安徽地区地震地质、历史地震活动研究等方面取得了一定的进展。
Studying on seism and geology and historical earthquake activity obtained some advancement in Anhui recent years.
首先根据历史地震目录，计算了我国34个省会城市所受到的历史地震影响。
Firstly, the impact of historical earthquakes on 34 China province level capital cities are evaluated by using historical earthquake catalog.
根据活动构造参数估计地质地震活动性，能克服历史地震记载时间短的局限性。
Geological seismicity estimated from parameters of active tectonics will overcome the limitation of short historical records of earthquake occurrences.
利用新疆历史地震考察资料，采用多元回归方法拟合新疆地区地震烈度衰减规律。
Combined with the survey data of historical earthquake in Xinjiang, the seismic intensity attenuation law has been fitted with multiple regression method.
历史地震研究几乎全部取材于史料，而方志中的地震记载又占了地震史料的绝大部份。
All study of historical earthquake is almost obtained from various historical materials, and earthquake records in local records hold most of historical earthquake materials.
结果表明，时间可预测模式比滑动可预测模式更接近胶辽海峡历史地震的时间序列特征。
The conclusion is that the time predictable model is more closer to the time series character history earthquakes than the slip predictable model.
由实际记载资料进行历史地震影响状况评价，并复核确认破坏性地震的震中位置和强度。
Evaluate the influence of historical earthquakes on the basis of actual records, review and identify the epicenter location and magnitude of destructive earthquakes.
这意味着本方法可以应用于推断某些历史地震的断层类型、破裂传播速度及破裂传播方向。
This suggests that the present method could be applicable to some historical earthquakes with known seismic intensity distribution to obtain detailed information on the faulting process.
同时，由该区域的历史地震(1300 ~ 1993年)可得到较大震级的实际年频次。
At the same time, the real annual occurrence rate on larger magnitude can be calculated by the historic earthquakes (1300 ~ 1993) recording in the same region.
本文综合了区域地震地质、历史地震和库区水文地质条件，概述了该区域的孕震构造背景；
In this pap. er, we described the seismogenic structure background by the synthesis of the regional seismogeology, historical earthquake and hydrogeologic conditions of the reservoir area ;
本文根据历史地震资料按最大熵谱方法对全球及全球各地震区强震活动的时间序列进行了分析。
Based on the historical seismic data, we have analysed the time sequence of the global and regional strong earthquake activities by using the maximum entropy spectrum method.
当一次中强地震发生后，用户需要迅速得到震区的历史地震信息以及与本次地震相关的一些信息。
When a moderate strong earthquake happens, users have to obtain history earthquake information of this area and relative information of this earthquake.
我们根据历史地震资料，采用统计学方法研究了川滇地区7条活动断裂带整体的强地震复发特征。
We use statistical methods to study the recurrence behavior of strong earthquake on entireties of 7 active fault zones of Sichuan-Yunnan region based on historical earthquake data.
文中研究了北京及其周围地区的历史地震和地震地质资料，并在此基础上估计了基岩运动的参数。
The historical earthquakes and seismotectonic data of Beijing and surrounding areas are described based on which parameters of input excitations of the basement rocks have been evaluated.
对于历史地震资料，准时间可预报复发行为可由地震后平静时间的对数与地震烈度的回归方程描述。
For historic earthquake data, this behavior can be described by the regression equation of logarithm of quiet time after an earthquake versus intensity of this earthquake.
根据历史地震记载、近期地震活动性和构造应力场资料，分析了北京西北延庆-怀来盆地的潜在地震危险性。
The potential seismic risk in the Yangqing-Hualai basin, NW of Beijing City, is estimated using historical documents and recent seismicity and tectonic stress field data.
通过实地考察和分析，结合历史地震记载资料，对熊耳山地貌、裂谷以及崩塌遗迹的形成原因进行了初步探讨。
Through field investigation and analysis, combining with historical earthquake documents, the causes of landform, rift valley and landslip relic of Xionger mountain is studied.
本文介绍并完善了作者提出的一种根据历史地震资料估计走滑断裂带地表断层平均滑动速率的方法：“均一滑动法”。
In this paper, a method, the uniform slip method, estimating average slip rate along surface trace of strike slip fault zone by historical earthquake data is offered.
本文介绍并完善了作者提出的一种根据历史地震资料估计走滑断裂带地表断层平均滑动速率的方法：“均一滑动法”。
In this paper, a method, the uniform slip method, estimating average slip rate along surface trace of strike slip fault zone by historical earthquake data is offered.
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