沉积盆地侵入岩区的异常“温度场、压力场和地球化学场”与油气的关系——以东营凹陷纯西辉长岩为例

通过岩石学、有机地球化学等分析 ,发现纯西辉长岩周围烃源岩具有有机质含量极低、高熟和裂缝发育以及油气比较丰富等特征 .研究表明 ,其根源是辉长岩形成的特殊温度场、压力场和地球化学场 ;辉长岩形成的异常高温大大促进了烃源岩热演化 ,并提高了生烃量 ;高压产生的大量裂缝为烃源岩排烃和油气聚集提供了通道和储集空间 ;而辉长岩带来的深源氢对烃源岩起到加氢作用 ,扩大了生烃量     

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.     

东营凹陷八面河地区坡折带特征及其对地层岩性圈闭的控制作用

通过对东营凹陷八面河地区广利东洼陷边缘坡折带的识别标志、成因机制以及演化规律的研究,总结了该区坡折带对于地层岩性圈闭的控制作用,以便为地层岩性油气藏的勘探提供依据.研究表明,该区广利东洼陷边缘发育挠曲坡折带和断裂坡折带,构造活动是形成坡折带的主要因素.坡折带的演化规律与构造活动的阶段性演化或幕式构造作用相对应,也表现出多期性、幕式活动和差异性活动的特点,而且坡折带规模与构造活动大小有关.坡折带对地层岩性圈闭的控制主要表现为:坡折带附近是地层岩性圈闭发育的有利区带;规模较大的坡折带控制了多数地层岩性圈闭,地层岩性圈闭在纵向上发育具有继承性特点;坡折带在横向上可以存在较大的变化,可形成不同的圈闭类型;坡折带控制下的地层岩性圈闭含油气性十分有利.     

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     

东营凹陷沙三段-沙二下亚段T-R层序特征及成因

将东营凹陷古近系沙三段沙二下亚段划分为 3个三级层序 ,即沙三下层序 (SSⅠ )、沙三中层序 (SSⅡ )和沙三上沙二下层序 (SSⅢ )。SSⅠ和SSⅡ层序由湖进体系域和湖退体系域组成T R旋回 ,其特征是代表层序边界的不整合分布局限 ,湖进体系域厚度小 ,主要为细粒沉积物 ,退积式叠加 ;湖退体系域较厚 ,由进积式叠加的砂岩、砾岩和泥岩组成。T R层序的形成主要是由于层序形成早期的构造沉降和气候起主导作用 ,其基底快速沉降 ,湖水供应充分 ,湖平面快速上升。在层序形成晚期 ,沉积物供给和气候起主导作用 ,沉积物供给多 ,快速向前推进 ,湖平面下降。构造沉降和沉积物供给因素对层序控制作用的转换促使其形成层序和体系域的边界。T R层序与三分层序之间的转换是由于层序形成的不同阶段的主控因素不同而引起的