华东某些山区第四纪古纬度变化

据１８８个古地磁样品和样品产地的地理坐标、余纬度、平均磁偏角和磁倾角，求得样品产地的古纬度．本区古纬度比现今纬度低：７．６°－８．２°，６．６°－６．８°，６．０°－６．５°，２．３°－３．４°，０．２°－０．６°．变化由印度板块和太平洋洋壳北推合力所致．     

A SPECTRUM OF LYAPUNOV EXPONENTS OBTAINED FROM A CHAOTIC TIME SERIES

A complete spectrum of Lyapunov exponents (LEs) is obtained from 1970— 1985 daily mean pressuremeasurements at Shanghai by means of a correlation matrix analysis technique and it is found that there exist LEs≥0,and <0. with their sum 0λ_i=K=0.110405 whereuponT=1 /K =9 is obtained as the predictable time scale, a result close to that acquired by the dynamic-statistical approachin early days and also in agreement with that present by the authors themselves(1991).     

离石断裂带的构造及其地震危险性

在山西断陷带西侧吕梁隆起的西坡上,有人认为有一条纵贯全区的离石断裂带,并把其作为鄂尔多斯断块和太行山断块的分界断裂,本文通过近期的工作结果及对深部构造、岩浆活动和钻孔资料的分析,认为把离石断裂带作为构造单元的分界断裂的依据不足。     

1990年10月20景泰地震的活动图象及其特征

本文研究了甘肃景泰6.2级地震的活动图象及其特征。该次地震的类型属主震余震型。其地震活动的特征表现为:强震前中小地震活动图象发生变化,临震前出现中小地震活动条带;震前中小地震活动时间分维值下降并出现最低值;该次地震发生于6级地震等间距分布的格局中,并呈现明显的补位特征。本文还提出了一种利用震级测定值最大的台站的方位,确定地震破裂面的方向和节面展布的方向的方法。     

On the seismic regime network method

In this paper, based on the previous study of practical use of seismic regime windows and seismic regime belts, the problem of establishing a “seismic regime network” consisting of “windows” and “belts” is further posed and discussed according to the observed fact that many “windows” and “belts” make responses to one earthquake. For the convenience of usage, the “seismic regime network” is divided into two classes, the first class and the second one. The former can be used in tendency prediction for long-term seismic activity in a large area, the latter used in short-term prediction in a small area. In this paper, after briefly discussing the physical significance of “seismic regime network”, it is pointed out that this simple and easily used method can be used to observe and extract seismic precursory information from a large area before a great earthquake, thus it can provide a reliable basis for the analysis and judgement of seismic regime tendency in time and space. No doult, this method is of certain practical significance. The Chinese version of this paper appeared in the Chinese edition ofActa Seismologica Sinica,13, 161–169, 1991. The English version of this paper is improved by Prof. Shaoxie Xu.     

计算伸展断层底界面深度的作图法简介

本文简介了计算正断层底界滑脱面深度的3种几何作图法。其中,M.W.Kilsdonk(1989)在Davison(1985)方法基础上作出的修正方法,简便且较准确。运用这种方法计算的鲁西地区深层次滑脱面深度与壳内低速层深度吻合。     

太平洋中部微生物与多金属结核的生成关系

作者采用洋底水-岩-微生物相互作用系统的观点首次对太平洋中部洋底多金属结核开展了微生物成矿作用的研究。通过洋底各介质中微生物活动与多金属结核生成机制、成矿物质转化的微生物作用及化学作用对比模拟实验研究、观察和测定系统中成矿物质浓度及环境参数的变化,揭示了成矿组分由微生物活动引起的反应速度和演变方向;从微生物地球化学作用的观点,论证了多金属结核微生物成矿机制和成矿模式;提出了多金属结核微生物成矿阶段和成矿理论。     

玲南金矿的成矿特征及断裂控矿规律研究

在对玲南金矿床的成矿特征、控矿构造、矿化及蚀变产物综合分析的基础上,论述和总结了矿床地质特征、破头青断裂带特征及其对成矿的主导控制作用。认为矿化和蚀变产物的形成在时间上相近、空间上叠加;它们是同一成矿作用的两个有机组成部分,是矿床成矿演化历史的实物记载;成矿期断裂的多次活动及第Ⅱ、Ⅲ阶段矿化的叠加发育,分别为玲南特大型蚀变岩型金矿成矿的必要条件和充分条件。