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。     

论华南栖霞组中的菊花石

本文中的菊花石指华南栖霞组中由柱状晶体放射状排列而成的菊花状晶簇。它最早发现于湖南浏阳永和镇栖霞组上部(方邺森等人,1988),之后又见于广西来宾县城郊栖霞组上部(沙庆安等人,1990),它们被认为是天青石或天青石假象。笔者(1991)在湖北省黄石地区栖霞组上部发现该类假象,并认为其原生矿物是六水碳钙石。虽然它们分别被解释成不同矿物,但无论是外部形态还是内部成分、结构构造均具极大的相似性。对该矿物集合体的不同解释将对栖霞组沉积环境的认识产生重要影响。本文通过与六水碳钙石假象的对比,讨论该矿物集合体的成因及其环境意义。不妥之处请批评指正。     

On the Development of Meso-Scale Heavy Rain Parcels in China

Heavy rains occur in China frequently, which often bring us floods and serious disasters in the summer half-year. The meso-scale heavy rain parcels (MHRP) in the mid-latitude are usually developed in following cases:I.By the approaching, meeting and / or overlapping of different weather systems, when two or more different rainfall systems are getting to conjugate, some MHRPs could be developed, such as: 1) a new cold/warm front or squall line approaches an old front or squall, even when the old one is somewhat decrepit; 2) at the places where two or more synoptic systems with different characteristics are meeting together, such as the meeting of tropical cyclone with the cold airs coming from the mid- and / or high-latitudes, or the low latitude vortex meeting with the westerly trough; 3) at the intersections of some different weather systems, such as the intersection of drylines, squall lines or fronts moving from different directions; and 4) by the overlapping of rainfall parcels produced continuously     

西太平洋区域二甲硫酸及其他硫化物的模拟研究

本文利用一维光化学模式，以二甲硫醚（ＤｉｍｅｔｈｙｌＳｕｌｆｉｄｅ，简称ＤＭＳ）为源模拟了西太平洋对流层的硫化物循环。ＤＭＳ海－气通量由“ｓｔａｇｎａｎｔ－ｆｉｌｍ”模式进行计算。尽管海洋大气中ＯＣＳ浓度比ＤＭＳ大一个量级，但它对ＳＯ２的贡献很小，ＤＭＳ仍是海洋大气中ＳＯ２的主要源。在大气垂直湍流输送过程中，ＤＭＳ白天与ＯＨ反应，夜间与ＮＯ３反应被氧化成ＳＯ２，ＳＯ２大部分通过非均相转化形成Ｈ２ＳＯ４。模拟结果与ＰＥＭ－ＷＥＳＴ－Ａ观测资料对比，取得了较好的一致性。