济阳坳陷红柳地区构造坡折带层序地层学模式与含油气性的关系

在对地震、测井和钻井等资料详细分析的基础上，将济阳坳陷红柳地区在下第三系划分出了7个三级层序，19个体系域．其中层序Ⅰ、层序Ⅳ为两个T-R层序分为两个体系域，即湖扩展和高位体系域，其他层序均为三分层序，划分为三个体系域即低位、湖扩展（水进）和高位体系域．在层序地层单元划分和对比的基础上，结合断层上下盘地层厚度的差异和地层厚度的变化反映古地形，认为济阳坳陷红柳地区在下第三系沉积时期，发育两种不同类型的构造坡折带，并建立了该区的构造坡折带层序地层学模式，研究了构造坡折带层序地层学模式与含油气性的关系，认为第Ⅰ、Ⅱ层序间的界面附近可形成有利的地层不整合覆盖圈闭与构造一岩性圈闭；第Ⅳ层序低位域可作为油气的运载层，在合适构造的匹配下，可形成有利的构造圈闭或构造-岩性圈闭，对有利区带做出了预测．     

Thermotropic copolyamides from triethyleneglycol bis (4-carboxyphenyl) ether,aromatic diamines,and p-aminobenzoic acid

It is proposed that depression of the transition temperatures, especially the melting point (T_m), can be achieved by the introduction of a different amide bond structure into the copolyamides of dicarboxylic acids and diamines by copolymerization of aminocarboxylic acids, such as p-aminobenzoic acid. The effect was examined by the amount and distribution of the structure in the copolylamindes. Copolycondensations of PEG₃, p-aminobenzoic acid, and diamines with different chain lengths showed that the structural change of the amide bond in the copolymers, especially its distribution, was more important than its total amount in them. Several types of aminocarboxylic acids were briefly examined to study the effect. © 1994 John Wiley & Sons, Inc.     

基于脑涨落图和抑郁评分系统评价中医综合治疗抑郁症的疗效

以DEP患者作为研究对象,利用脑涨落图仪（EFG）的客观检查方法及DEP现代医学评分系统,评价解郁合欢汤+五行音乐疗法的中医综合治疗方式对DEP的疗效。指标包括EFG检测大脑神经递质相对功率值、汉密尔顿抑郁量表（HAMD）以及蒙哥马利抑郁评定量表（MADRS）。EFG结果显示,患者治疗后脑内γ-氨基丁酸的相对功率值较治疗前显著降低（P<0.001）,去甲肾上腺素（P<0.001）、多巴胺相对功率值（P<0.001）较治疗前显著提高,患者治疗后的HAMD(P<0.001)、MADRS(P<0.001)较治疗前显著降低。说明中医综合疗法对DEP的疗效确切,可通过对大脑神经递质的调节作用而发挥抗抑郁疗效。     

Salting-in of alcohols in aqueous solutions by tetraalkylammonium bromides at the freezing temperature

The freezing-point depression of the ternary systems tetraalkylammonium bromides-t-butanol-water for the first five homologs of R₄NBr was measured. In the case of Bu₄NBr, the effect of size of the alcohol (methahol ton-butanol) was also investigated. From the corresponding freezing-point data for the binary systems the apparent salting constants were calculated. The true salting constantsk _s were obtained by extrapolation to infinite dilution. These are all very close to zero at the freezing temperature. From the corresponding thermochemical data the temperature dependence ofk _s was calculated, and above 5°C all the R₄NBr salts int-butanol; the salting-in increases with temperature and with the size of the hydrophobic cations. The scaled-particle theory is at present the only one which can account semiquantitatively for the temperature dependence of the salting-in effect. On leave of absence from Chemistry Department, The University, Sheffield S3 7HF, England To whom correspondence should be addressed.     

IDENTIFICATION OF LANOSTANES AND THEIR POSSIBLY GEOCHEMICAL SIGNIFICANCE IN BIYANG DEPRESSION

In the study, a series of C_(30)-C_(32) lanostane homologs have been identified from Eogene source rocks and crude oils of Biyang depression in Henan Province, China. Based upon the geochemical investigations and simulating experiments, the idea that the generation of lanostane may mainly be related to the specific original organic inputs and low maturity has been proposed.     

FORMATION AND DEVELOPMENT OF TAIHU LAKE AND RECENT DEPOSITION

Situated in the Taihu plain between the mouth of the Changjiang River and theHangzhou Bay, the Taihu Lake is a large shallow-water lake in China with a surface area of 2427.8 km~2.The lake bottom mainly consists of loess-like sediment. Some buried and silted up channels and residual depressions can be found at the bottom and a lot of Neolithic cultural relics on the loess-like sediment. This indicated that the Taihu Lake was formed on the alluvial plain charaterized by widely deposited loess-like sediment because of siltation and stagnancy of water, instead of by development from lagoons as reported in the past.Recent deposition including influent-effluent current accumulation, wind-driven current and storm deposition in this lake occurred mainly in the south, the west shore and the midst of the lake.The sedimentary rate in the east Taihu Lake is about 1.7-1.8 mm/a, whereas in the west Taihu Lake it is about 0.41 ram/a, only 23％ of that of the former.     

惠民凹陷古近系碎屑岩储集体成因类型及特征分析

对惠民凹陷在古近系碎屑岩储集体的成因特征进行了分析研究.发现成因类型有:冲积扇、河流、近岸水下扇、扇三角洲、深水浊积扇、三角洲、三角洲前缘滑塌浊积扇以及滨浅湖滩坝.储层岩石类型有砾岩、含砾砂岩、中细砂岩及粉砂岩.不同成因类型的碎屑岩储集体成分成熟度和结构成熟度差异较大,三角洲河口坝及滨浅湖滩坝砂体成分成熟度和结构成熟度最高.不同成因类型储集体的物性特征不同,三角洲平原分支河道、(扇)三角洲前缘水下分流河道及河口坝砂体储集物性最好,其次为(扇)三角洲前缘席状砂及滨浅湖滩坝砂体,近岸水下扇和浊积扇砂体物性相对较差.     

辽河盆地东部凹陷北部地区Es1+2/Es3不整合面与油气运聚的关系

根据 2 2 4口井的实际资料 ,结合地层沉积特征和地震剖面解释结果对辽河盆地东部凹陷北部地区Es1+ 2 /Es3 不整合面的上、下地层的接触关系及岩性组合特征进行了平面规划及分类 ,探讨了该不整合面与油气运聚的关系。研究结果表明 ,不整合面在油气运聚过程中所起的作用主要是由不整合面上、下地层的接触关系及岩性配置所决定。研究区凹陷北部茨 5 9井—茨 80井、龙 12井—龙 2 4井等区域为寻找不整合面之下遮挡油气藏的有利地区 ,茨 6 7—茨 6 15区域是该不整合面之上油气聚集的有利区     

济阳坳陷上第三系馆陶组河流相沉积的粒度特征

讨论了济阳坳陷上第三系馆陶组河流沉积的粒度特征，在对１４口岩心井３００块样品粒度分析的基础上，研究了粒度参数与水动力条件之间的关系，总结归纳出不同微相的概率曲线特征，并利用Ｃ－Ｍ图、萨胡判别式和粒度离散图研究了河流类型．研究结果表明，不同性质的河流，其粒度在垂向上的变化速率不同，直接影响到砂体的非均质性．     

飞雁滩油气田明下三段沉积微相研究

从岩心观察入手，综合运用地质、测井曲线及测井资料数字处理成果，详细研究了飞雁滩油气田明下三段的沉积微相类型及其平面展布特征，研究结果表明，飞雁滩油气田明下三段属曲流河沉积，可细分为河道、河道边缘、废弃河道和洪泛平原四个亚相。其中．主要发育废弃河道和洪泛平原两个亚相。这两个亚相又可进一步细分为废弃河道、废弃河道边缘、河漫滩地和河漫洼地四个微相，由构造特征及少量的试气资料分析发现，天然气主要分布于废弃河道微相中，其次是废弃河道边缘微相和河漫滩地微相，河道边缘亚相是较有利的储集相带。