波动地质学研究中资料的收集与整理

波动地质学是进行盆地定量分析的重要理论之一，本文结合黄骅坳陷实际工作经验和成果，详细介绍了波动地质学研究中资料收集、整理的基本过程和原则．阐述了资料准备工作在波动分析中的重要作用。根据黄骅坳陷的地质条件，将坳陷划分成９个研究小区，进行了岩性厚度剖面向岩性对间剖面的转化；恢复了各组段的原始地层厚度和沉积速率；利用滑动窗口绘制了沉积速率曲线并建立了相应的波动方程，得出了东营时期坳陷抬升的扩散过程，研究声明，钻井资料的收集、整理和地层厚度的恢复是波动分析成败的关键，而滑动窗口的运用是实现定量分析的重要纽带。     

湖泊扇三角洲的重要特性

湖泊扇三角洲作为重要的油气储集体广泛分布于我国东部含油盆地中，文章在分析湖泊扇三角洲形成条件的基础上，指出扇三角洲发育前缘席状砂，阐述了湖泊扇三角洲的岩性、结构、沉积构造以及地球物理特征，建立了区域生沉积模式。研究表明，前缘席状砂是良好地油气勘探目标。     

平顶山煤田山西组沉积体系与聚煤模式

讨论了河南平顶山煤田山西组的沉积体系和聚煤模式。文中提出山西组下段形成于碎屑障壁海岸环境,山西组上段为三角洲沉积体系的进积部分。已组煤形成于障壁海岸沉积体系的上部,其发育过程明显受到基底沉积环境的控制。已组煤的聚煤作用特征是沉积基底地形高差、压实沉降率与泥炭堆积速率之间的平衡关系随海平面变化而变化。己组煤发育的气候条件可能属热带背景。     

平庄西露天矿区元宝山组沉积体系分析

本文运用现代沉积学原理和方法．以丰富的地质资料为基础，把西露天矿区元宝山组自下而上划分为湖泊三角洲体系和扇三角洲体系、冲积扇体系、曲流河体系、辫状河体系．比较详细地剖析了各沉积体系的构成、特征，再现了聚煤期及其前后的沉积环境演化。     

云斑天牛生殖系统的研究

研究了云斑天牛生殖系统的解剖形态、超微结构及内、外生殖器结构的功能和组织来源。     

用多距离特征识别三维物体的表面形状

本文讨论一种识别物体的方法。三维空间中的物体表面可以由部分球面、柱面和平面来近似,并且这些面是能够被识别的。处理方法是通过分割图象成为区域(Region)且并行处理这些区域来实现。文内叙述一种技术。这种技术应用具有激光扫描器的摄象机系统获取图象。测量三维物体相应表面点的座标。然后用相应区域中的三点决定一个参考平面,进而计算区域中的特征点到参考平面的距离。这些多距离特征可被用来识别相应区域中的物体表面是球面、柱面还是平面。这些面的方向,可用具有两个斜角的表面法线方向来描述。这种技术在自动装配线上和工业监视检验中是很有用的。可用其找出另件在三维空间中的位置和方向,计算检验另件表面形状外形尺寸等等。     

Linear sand ridges on the outer shelf of the East China Sea

Based on the latest full-coverage high-resolution multi-beam sounding data, the distribution of the linear sand ridges on the outer shelf of the East China Sea （ECS） is studied with quantitative statistical analysis. The study area can be divided into the northeastern part and the southwestern part. Sand ridges in the northeastern area, trending 116°N, show obvious linear character and shrink to the inner shell Sand ridges in the southwestern area, trending 120°N -146°N, tend to have net form. Sand ridges gradually become sand sheets in the center part of study area. Sand ridges are distributed landward to the isobath of 60m, distributed seaward to the water depth of 120 m in the northeast and 150 m in the southwest. Immature sand ridges are observed at water depth of 130-180 m in the southwestern depressions. The acoustic reflection properties of the internal high.angle inclined beddings of the sand ridges are analyzed based on the typical seismic profiles close to the research area. Lithological analysis and dating of 4 boreholes and 12 cores indicate that the widely distributed transgressive sand layer with high content of shell debris which was formed in the early-middle Holocene is the main composition of the linear sand ridges on the outer shelf of the ECS. The dominating factor in formation, developing and burying of the sand ridges is the variation of water depth caused by sealevel change and the rate of sediment supply. In 12400 aBP the cotidal lines of the M2 tidal component were closely perpendicular to the strike-directions of the sand ridges in the study area, and the tidal wave system during 12000-8000 aBP might play a key role in the formation of the linear sand ridges which are widely distributed on the outer shelf of the ECS.     

300 MW 直接空冷汽轮机的结构特点

鉴于空冷技术的广泛运用,空冷汽轮机相继投入运行。概述了300MW空冷汽轮机系统结构,并简要对直接空冷原理及流程进行了说明,分析了300MW直接空冷汽轮机与湿冷汽轮机在结构、系统方面的差别,以便为300MW空冷汽轮机的安全运行提供帮助。     

大鳞鱼巴形态特征测量与分析

对乌兹别克斯坦引进的大鳞鱼巴鱼3 龄,1 龄,1-龄共11尾的形态性状进行测量.结果表明,全长/体长为1.16~1.22,体长/体高为5.00~5.57,体长/头长为4.50~5.33,体长/尾柄长为4.69~6.15,头长/吻长为3.14~3.38,头长/眼径为4.64~12.5,头长/眼间距为2.43~2.82;背鳍Ⅱ为7~8,腹鳍Ⅰ-Ⅱ为8~9,胸鳍Ⅰ为13~18,臀鳍Ⅰ-Ⅱ为5~6,尾鳍为20~24,侧线鳞为72~73,鳃耙为20~28,咽齿3行,脊柱数量44~45,无幽门盲囊,尾鳍形状正尾型,鳔2室.     

Fractal Characteristic of Soil in Typical Debris Flow.Triggering Region： A Case Study in Jiangjia Ravine of Dongchuan, Yunnan

The structural features of soil in debris flow-triggering region play an important role in the formation and evolution of debris flow. In this paper, a case study on the fractal of soil particle-size distribution （PSDFs） and pore-solid （PSFs） in Jiangjia Ravine was conducted. The results revealed that the soil in Jiangjia Ravine had significant fractal features and its PSDF and PSF had the same variation trend despite different type of soils in debris flow-triggering region： residual soil （RS） 〉 debris flow deposit （DFD）~clinosol （CL）, their fractal dimension of PSDFs are respectively between 2.62 and 2.96, 2.52 and 2.68, 2.37 and 2.52; and the fractal dimension of PSFs are respectively between 2. 75 and 2.95, 2. 57 and 2. 72, 2.59 and 2.64. The fractal dimension of soil reflected its complexity as a self-organizing system and was closely related to the evolution of soil in debris flow- triggering region.