皖南东至地区寒武系层序地层研究

皖南东至地区寒武系在地层分区上可以分为下扬子地层分区、过渡地层分区和江南地层分区，生物群上出现了两区特征分子和过渡区的混生现象，并处于台地与盆地交接部位。通过对分别位于台地、斜坡和盆地露头层序地层研究，将寒武纪地层自下而上划分为三个Ⅱ类沉积层序和二个Ⅰ类沉积层序，早寒武世的三个Ⅱ类沉积层序的陆架边缘体系域不发育；中寒武世晚期到晚寒武世的二个Ⅰ类沉积层序皆由低水位体系域、海侵体系域和高水位体系域 组成三元结构。通过层序地层分析和沉积体系演化建立了相应的海平面变化曲线，自早寒武世早期本区海平面达到最高位和最大上升速率后，至寒武纪末研究区海平面总体处于下降过程，即海平面为累进式的缓慢的下降。     

区域发展限制性因素的探讨—以湛江市为例

几十年的研究与实践表明，区域发展要“扬长避短”，即要重视区域优势的发挥，也要注重区域发展的限制因素。在实地调查的基础上，以湛江市为例，强调了区域发展限制性因素研究的重要性。认为湛江市的区域发展在区域政策、区域组织、区际联系和区域管理等方面都存在着问题，这些问题在很大程度上阻碍了湛江市的区域发展。湛江市经济实力不强、区域发展水平低，产业结构不合理、工业发展长期滞后，主导产业的产业关联度不强，经济次益欠佳，限制性因素的负面效应非常明显。必须从限制性因素的弱化与克服方面入手，立足资源优势、合理确定经济发展政策，适当调整行政管理体制、提高行政效率，深化现代企业制度的改革、提高企业经济效益，重视城市形象工程建设，改善投资环境，才能改善湛江市区域发展的不利局面。     

新集二矿下夹片地层特征及在防水煤柱留设中的意义

针对新集二矿新生界松散层，推覆体下开采的特殊地质及水文地质条件，通过对夹片地层水文工程地质条件，边界条件及富水性特征的分析，阐明夹片地层在防水煤柱留设中的意义，并通过生产实践验证，取得了较好的经济及技术效益。     

Arnol'd Nonlinear Stability Theorems and their Application to the Atmosphere and Oceans

Within the context of atmospheric and oceanic fluid dynamicsthe problems of nonlinear stability and instability, particularlythe Arnol'd second type nonlinear stability, are surveyed.The stability criteria obtained by means of the energy-Casimirand energy-Lagrange methods are presented for a varietyof models, the estimates for various generalized perturbationenergy and enstrophy are given. Potential applications of thesecriteria are shown in the estimation of bounds on the perturbationenergy and enstrophy, in the diagnostic study of the persistence orbreakdown of jet flows in the middle and high latitudes, and in theverification of the validity of the tangent linear model in bothatmospheric dynamics and oceanography.Some further research results are also highlighted.     

A discussion on the application ofb-value to the prediction of seismic tendency

In the estimation of seismic tendency, using Gutenberg-Richter’sb-value and using Hurst exponent are two commonly used methods. Based on the fractal geometry of earthquake time series, we point out that these two methods correlate to each other. In the perspective of fractional Brownian motion (FBM), an earthquake sequence withb>3/4 and that withb<3/4 have different dynamic properties. Foundation item: The MOST Project G1998040705. Contribution No. 01FE2010, Institute of Geophysics, China Seismological Bureau.     

块状硫化物矿石中硫化物的压溶和增生及成矿意义——以加拿大西部矿床为例

加拿大西部块状硫化物矿石普遍地发生过硫化物的压溶和增生。增生作用根据增生体的成分可以分为同质增生和异质增生，根据动力环境可以分为静态增生和动态增生。三晶嵌接结构可以是静态增生的产物。压溶和增生是块状硫化物矿床成岩和变质过程中的重要作用。脉石矿物的压溶可使原生矿石就地加富，硫化物的压溶可使成矿物质发生再活化。增生可促进矿质沉淀。富含硫化物的地层之所以能成为地球化学障而有利于后期热液叠加和层控矿床的形成，硫化物晶芽的增生是一种重要机制。     

地质异常理论在兰坪盆地演化中的应用

基于地质异常理论的分析，并结合兰坪盆地的地质、构造特点，充分发挥地壳升降系数法的定量化及其空间优势，对兰坪盆地地质、构造演化进行了形象、直观的表述，对进一步反演兰坪盆地独特构造格架形成的古应力场，具有十分重要的作用。     

Study on the relationship between geothermal exploitation and seismic activity in Xi’an region

Based on the analysis of the induced earthquakes in China and abroad, we get some ideas about earthquakes induced by pumping water out of a well or injecting water into a well. The induced earthquakes usually occur near the well, and they are generally small earthquakes. The earthquake sources are shallow, and they belong to the main shock-after shock type of earthquake or the swarm-type of earthquake. The magnitude and the quantity of the induced earthquakes obviously depend on the pressure and the quantity of water pumped or injected. These earthquakes happen as soon as pumping or injecting occurrence, or after ten or twenty days, they may occur at the time of injecting mud or injecting high pressure water when a well is being drilled, or at the time when the ground water is being normally exploited. A large quantity of hot water has been exploited since 1990 in Xi’an, and the quantity of water exploited has been increasing year by year, as a result the groundwater level has been dropping with the water pumped out and the water level is high in summer and low in winter. The earthquakes in Xi’an region belong to the solitary-type and they spread outside Xi’an city where the wells are concentrated but no earthquake happens. The seismic frequency and the energy released have no relation with the quantity of water exploitation or the water level in the well. It is considered that geothermal exploitation does not induce earthquakes in and around Xi’an because of its specially geological condition. Foundation item: Project sponsored by the Landslide Office of Shaanxi Province and Society of Disaster Reduction of Shaanxi Province.     

Characteristics of surface ground motions induced by blasts in jointed rock mass

An in-situ experimental program in a jointed rock mass was designed and implemented to investigate the rock joint effects on stress wave propagation. Accelerometers were placed on rock surface along three lines at 0, 45 and 90° to the predominant rock joint strike direction. Eight blasts were detonated in a charge hole drilled in the rock mass. The equivalent TNT blast weight ranged from 2.5 to 50.0 kg and the loading density (charge weight divided by the charge chamber volume) varied from 1 to 20.0 kg/m³. A fully coupled detonation with a charge weight of 25.0 kg was also exploded to study the coupling effect. The recorded data are presented and analyzed in this paper. The effects of rock joints on characteristics of stress wave propagation such as peak value attenuation, spectrum, and spatial variations are discussed.     

北祁连石居里地区Cu(Zn)-S矿床地质特征及综合成矿模式

文章主要论述了北祁连山西段石居里矿田内Ⅵ号沟、Ⅷ号沟、九个泉等矿床的基本地质特征，并与北祁连山东段老虎山地区银硐沟、猪嘴哑吧等矿床对比。结合其早古生代构造演化历史、古洋脊或弧间、弧后拉张环境确定矿床类型，将上述3个矿床归属为蛇绿岩Cu(Zn）－S型矿床（类塞浦路斯型）。建立综合成矿模式的基本要求：（1）矿床具有一定的时控性，有一定的含矿层位；（2）生长性断裂的积极参与；（3）海底火山喷发、喷气中心与次级盆地双向控制；（4）多元热流体成矿系统。