跨断层形变测量场地图形分析及设计

在分析了青藏体北缘跨以形变测量场地图形状态的基础上,论述了进行优化设计的必要性及新的图形设计的主要内容：（１）以ＧＰＳ控制整个断裂、以水冷、测距、基线、重力等测量手段监测各个场地测点形成的三维地形物重力变化信息;（２）断层水准、重力按新的标石裂线阵设;（３）断层水平形变可根据运动状态的不同,按“走滑型”和“倾滑型”布设;（４）场地水冷、重力定期水准、重力联测,场地水平没距网定期与区域ＧＰＳ网联测,     

唐山地震孕育的卫星遥感信息及意义

用华北地区多时相、多波段陆地卫星图像,研究1976年唐山7.8级地震孕育过程中,电磁波辐射反映的构造活动信息的类型、时间、空间特征,探讨构造活动信息的属性,形成机理及意义。     

试析综合国力的构成要素

综述了综合国力的构成要素 ,并把它们分为 3种类型 ,即物质性因素、政府性因素和精神性因素 ,尔后分别对其进行实证分析。     

ISENTROPIC TRAJECTORY ANALYSES OF POLLUTANT TRANSPORT IN NORTHEAST ASIA-INFLUENCE ON CHINA FROM NEIGHBORING COUNTRIES

The transport of air pollutants from several big cities in the north of China and theneighboring countries is researched by using the isentropic trajectory model. The trajectories arecalculated twice daily for the cities in January, April. July and October for the period of 1992-1994. The statistical method has been used to deal with trajectory dots at intervals of 30 min forthe forward and backward trajectories during 0-24 h and 24-48 h. The probability distributiondiagrams of trajectory show clearly the ensemble properties of isentropic trajectories for each cityand the dominant transport directions of pollutants. They possess notable seasonal variations. Theforward trajectory areas of the Ulaan Baatar in Mongolia can spread over North China. and thoseof the Chita in Russia can influence Northeast China except in summer. In July the forwardtrajectory of Pyongyang and Seoul can extend northward to the boundaries of China.     

Features and physical process of the dynamic evolution pattern of ground resistivity precursor front

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Structural features of crust-mantle assemblage in the lithosphere along the longitudinal Seismic Belt of China and their tectonic effect

The 1° × 1° distribution map of crust-mantle structural ratio R for the lithosphere along the Longitudinal Seismic Belt of China has been compiled using computer based on the results of geophysical prospecting by previous researchers, and the latest results by the present authors. Based on this map, an insight into the structural features of the crust-mantle assemblage along the Longitudinal Seismic Belt has been gained, while their relation to seismic activity and the distributions of geothermal flux and intracrustal high conductivity-low velocity layers, as well as their tectonic effect to seismicity have been discussed. Contribution No. 97A0079, Institute of Geophysics, State Seismological Bureau, China.     

唐山地震发震构造的浅层地震探测

利用浅层地震探测方法,研究了唐山地震区１年前出现在卫星图像上的异常现象与发震构造的关系,探讨地震中长期预测的途径。结果表明：唐山地震断层是一条倾向ＮＷ的右旋走滑第四纪同生断裂,它错断了全新统,晚更新统,中更新统,和早更新统地层。     

马剑-下梓州断裂带特征及其对天姆尖盆地铀矿的控制作用

本文根据马剑-下梓州断裂带的基本特征,分析研究了该断裂带的形成和发展过程;同时根据该断裂带两侧已知铀矿化的特征,阐明了马剑-下梓州断裂带对铀成矿的控制作用。在初步查清天姆尖盆地铀成矿地质背景及其形成富大铀矿床若干地质条件的基础上,指出天姆尖地区寻找富大火山岩型铀矿的方向。     

卡诺图化简多函数的简便方法

本文讨论了利用卡诺图进行多函数化简的一种简便方法。     

复杂条件下的回剥反演方法——最大深度法

常规回剥反演方法仅能面对简单情况,对于地层多次隆升剥蚀和多时代连续剥蚀的复杂情况,计算起来十分麻烦,既难以按统一的方式进行处理,也难以实现回剥反演的自动化．提出了一种更适用的回剥反演法———最大深度法,其主要思路是始终寻找从古至今各时间柱中埋深最大的一柱进行回剥反演．该算法逻辑简单明了,回剥反演过程简单,能自动实现,并可方便地推广到三维空间,实现三维构造史模拟．通过某地区实际资料处理,表明该方法正确可靠．