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地震活动性

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Seismicity trend before the earthquake was forecasted according to seismicity feature and commensurable characteristics of strong earthquake activities of Sichuan and Yunnan areas.Since Oct., 1995, a lot of kinds of the anomalies with large amplitude, such as radon and CO2 contents in groundwater and groundwater level etc.synchronized in a wide range of western Yunnan, especially along Zhongdian—Nanjian seismic area. The characteristics of these short-term anomalies are introduced and analysed.

根据川滇地区地震活动特征和可公度性计算结果,在该次地震前对地震大形势进行了预测。1995年10月以后,滇西北地区出现了大面积、大幅度、多手段的同步异常,其中以水氡、水位和CO2异常为主,沿中甸─南涧地震区分布较为集中。

It was suggested that the risk of active faults can be reasonably explained by the history of the faults and their occurrence period,while the risk of groundsill seismic liquefaction was examined in the field with penetration test.

活动断裂的危险性主要根据断裂的活动时期、断裂不同部位的活动性以及评估区距离断裂活动部位的远近程度进行评估。地震砂土液化判别采用现场标准贯入试验进行评估。

Analyze and compare the seismic characteristic after impoundment in the initial project of Danjiangkou reservoir.

但是,当水位达到初期工程最高水位,并诱发了4.7级地震后,蓄水位和地震的相关性逐渐消失,地震的活动性明显降低。

By means of different subjects and te chniques,the paper makes an overall study on the crustal stability of Beihuaiyang region and its adjace nt areas from the aspects of current t ectonic stress fields,principal fa ult structures,analysis of regional fa ults and neotectonic activity,seis mic activity and numerical modeling,etc.

运用多学科、多技术相结合的研究方法,从现今构造应力场特征、现代地壳形变特征、主干断裂构造以及区域断裂活动性分析、新构造运动、地震活动、数值模拟等方面入手,对北淮阳及其邻接区地壳稳定性进行了全面而系统的研究,指出本区地震活动受走滑活动断裂控制,中、强地震集中于区内东南部和西北部NW向与NE向断裂交汇处;第四纪无大规模差异升降运动;数值模拟等综合分析表明,信阳地区的区域构造稳定性高,现代地壳形变量小,应力平缓,地震活动少且弱。

It is considered that the geotectonic background is complex and seismicity is relatively week in the area.

认为该地区地质构造背景较为复杂,地震活动性相对较弱。

The mechanical strength of the crust and the seismicity of geotectonic units were strongly affected by geothermal characteristics of the units.

研究表明,各主要构造单元的地壳力学强度和地震活动性均受其地热特征的影响。

The activities in different sections of the Gaoqing fault in the Huagou gas field were analyzed using 3D seismic data. The activities of the fault segment associated with the Huagou gas field were strong during the Guantao\|Minghuazhen period, while the activities on east and west sides of the gas field were weak at that time. The Huagou gas field is well corresponding to the strong activity segment of the Gaoqing fault on the plane. The process of gas migration in the Huagou reservoir is divided into two phases:(1)After mantle\|derived magmatogenetic gas including CO2, N2, and He entered the Gaoqing fault, the gas migrated to the top of the fault by the action of buoyancy or pressure, then the gravitative differentiation occurred. For the top of the fault is closed and both sides of fault is sealed, the gas assembled to some degree in the Gaoqing fault;(2)When gas was accumulated at a large scale in the Gaoqing fault, the gas migrated towards the reservoirs along the two sides of the fault and was accumulated in sandstone.

利用三维地震资料,对济阳坳陷花沟CO2气藏区高青断裂走向上不同区段的活动性进行了分析,指出:花沟CO2气藏所对应的高青断裂区段,在馆陶组—明化镇组沉积时期活动性强,而气藏的东、西两侧,馆陶组—明化镇组沉积时期断裂基本上不活动;花沟CO2气藏与馆陶组—明化镇组沉积时期高青断裂活动性强的区段在平面上有着良好的对应关系;花沟CO2气藏的运聚过程分为2个阶段,在第1阶段,幔源岩浆成因的CO2、N2和He等气体进入高青断裂后,在浮力或压差作用下向断裂顶端运移,并发生重力分异,由于断裂顶端封闭、两侧封堵,CO2、N2和He等气体在高青断裂中实现了一定程度的聚集,而在第2阶段,当CO2、N2和He等气体在断裂中聚集到一定程度,便在压力驱动下向断裂两侧砂岩储层运移,并在其中聚集成藏。

Major conclusions are given in the end of this paper,that seismic statistical zone bases on the result of seismic belt delimiting,it only arises in and can be used in the especial PSHA method of China with considering spatially and termporally inhomogeneous seismic activities,and its concept should be clearly differentiated from the comcept of seismic belt.

文中最后指出,地震统计区划分是以地震带划分研究为基础,它产生并服务于考虑地震活动时空不均匀性的概率地震危险性分析方法,应将其与地震带概念加以明确区分,并加强其划分原则、理论和方法的研究。

Second, there may be no permeable, well-oriented faults at these depths. This might be the proximity of the bottom of the hole to the brittle-ductile transition, even in this relatively stable interaplate area.

这个深度也可能是这一区域内的地震活动性的最大深度,或者说是在这样相对稳定地区的板块内部,主井底已接近脆延性转换带。

In this paper,the relations between isostatic gravity anomaly in Fen-Wei fault depression zone,surfacial tectonics,crustal stracture, neotectonic movement and seismic activity are discuseed.

本文研究了汾渭断陷带均衡重力异常分布特征与地壳表、浅层结构,新构造运动和现代构造运动,以及均衡重力异常与地震活动性之间的关系。

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