1995年4月15日营口高坎M＿L5．0地震概述

１９９５年４月１５日营口高坎Ｍ＿Ｌ５．０地震，震中区烈度达Ⅵ度。总结发现，震前在一定的震兆异常背景上，出现一批短临前兆异常，如深井水位、水氡、水温、水汞、地倾斜、地电阻率、宏观等。分析认为，它可能是介质较薄弱的老震区对大区域应力场作用增强的反映，是我省震情发展中一次重要的地震事件。     

断层带土壤气的映震效能与地震短期预报

本文系统总结了首都圈地区（１１５．０°─１１７．５°Ｅ，３９．５°─４１．０°Ｎ）近３年来开展的断层带土壤气观测研究的结果，评价了断层气异常的映震效能，分析了映震特征，初步建立了地震短期预报的指标与方法。     

山西中强地震前形变前兆的异常特征

研究了山西地震带近年来数次中强地震前断层位移测量资料显示的异常变化，从背景异常、中期趋势异常和短临异常的不同角度讨论了震前地壳形变特征及应力场变化情况，得出了形变预报指标，并就有关问题进行了讨论。     

The multivariate controls of hydraulic geometry: A causal investigation in terms of boundary shear distribution

Most downstream hydraulic geometry exponents have been found to be very close to the classic values reported by Leopold and Maddock (1953). These have been viewed as the simplified cases to general trends because the hydraulic geometry of alluvial channels is actually the product of ‘multivariate controls’ (Richards, 1982). This paper is an attempt to develop a soundly based foundation for the explanation of the physical mechanisms of these controls. A quantitative relationship between channel shape and boundary shear distribution developed from experimental flume results is found to be applicable in some instances to alluvial channels, particularly to stable canals. On the basis of this relationship, it is shown that downstream hydraulic geometry is determined not only by flow discharge, but also by channel slope, channel average roughness and sediment composition of the channel boundary. This is strongly supported by our analysis of 529 observations from both stable canals and natural rivers in the U.S.A. and the U.K. The difference between regime relations in canals and the hydraulic geometry of rivers appears to be caused mainly by channel slope and average roughness, which can be regarded as constants only in stable canals. The close relationship between discharge and channel average roughness observed in canals is not repeated in natural channels, partly because of the variety of flow values used to define the channel-forming discharge. Furthermore, it is indicated that the effects of the sediment composition of the channel boundary on hydraulic geometry are significant and need further investigation.     

链子崖T_（11）—T_（12）缝段危岩体开裂变形机制

文章全面描述了链子崖Ｔ（１１）—Ｔ（１２）缝段危岩体的开裂形变特征，探讨了危岩体形成的影响因素，如重力、煤层采空区、降雨、水库蓄水、勘探掘进和地震等，指出其破坏机理是重力主导下的不对称的压力拱与悬臂梁（板）弯矩的联合作用。危岩体可以分成具有不同稳定程度的若干块体，治理工程也应针对它们的不同特点而设计。     

贡嘎山海洋性冰川发育条件及分布特征

贡嘎山５０００ｍ以上山体面积占全区总面积的六分之一，这样高大的山体为冰川发育提供了有利的地势条件和宽阔的积累区。同时，据观测推算东坡冰川积累区的年降水量可达３０００ｍｍ，雪线处的年平均气温在－４．１—－５℃；西坡冰川积累区的年降水量达１８００ｍｍ为本区冰川发育提供了丰富的冰雪物质条件和必要的低温。冰川形态类型基本齐全，冰川分布比较集中，但东西坡冰川在规模上有明显差异，东坡冰川条数较西坡少，但冰川规     

地层综合柱状图自动绘制的技术研究

介绍的软件及绘制技术成功地处理了地层综合柱状图中的化石、火成岩及相变等的绘制技术问题；其自动化程度高，具有很大的灵活性，以适应不同格式图件的要求。通过自编的接口软件由原始数据最终形成ＡｕｔｏＣＡＤ环境下的二进制图形交换文件。     

高级语言与AutoCAD共享地形图图式独立符号库的方法

本文在分析以AutoCAD形文件所建立的《地形图图式》独立符号库结构的基础上，提出了高级语音共享AutoCAD符号库的方法，并对该方法的实现过程作了详细的叙述．作者用TurboC程序设计语言编制了与AutoCAD绘图软件中shape命令具有相同功能的模块．