柴达木盆地西部第三系碳酸盐岩层的古生物特征

柴达木盆地西部第三系的碳酸盐岩层中发现有藻类、介形虫、有孔虫、腹足类、多毛类等化石.除藻类外各种生物的数量都比较少.生物具有个体小,壳体构造简单,多样性低等特点.所有生物都属于广盐性生物.根据该区古生物特征分析和与其它地区的对比,认为当时该区生物生长于内陆半咸化湖至咸化湖环境,而不是海相或海陆过渡相环境.参11.     

超重力场中微细晶须碳酸钙结晶过程及产品稳定性研究

在旋转填充床转子高速旋转产生的超重力场中，以MgCl12或H3PO4为晶形控制剂合成微细晶须碳酸钙，通过反应过程中pH值的变化以及针状晶种存在与否两种情形下晶体形貌的演变对结晶过程进行了研究，同时对产品粒子的稳定性进行了初步探讨．结果表明，无晶种存在时，微细晶须碳酸钙晶形的形成需要经历不规则外形-类纺锤形-晶须状-微细晶须状4个阶段；有晶种存在时，产品粒子倾向于在其表面或周围成核，最终所有粒子短轴与长径比趋向均匀；微细晶须碳酸钙粒子在陈化及干燥情形下表现出良好的稳定性．     

聚乙烯胺在CaCO3加填造纸中的作用效果

探讨了在弱碱性条件下聚乙烯胺(PVAm)对CaCO3加填的芦苇浆和废纸浆的助留助滤效果．实验结果表明：PVAm在两种浆中都有非常显著的助滤．助留效果，且在芦苇浆中的助滤效果大于废纸浆．PVAm在芦苇浆中对纤维的助留效果不如废纸浆，但对CaCO3的助留效果高于废纸浆．     

Discovery of the granulite xenoliths in Cenozoic volcanic rocks from Hoh Xil,Tibetan plateau

Two-pyroxene granulite and clinopyroxene granulite xenoliths have been recently discovered in the Late Paleogene toNeogene volcanic rocks (with ages in the range of 4.27～44.60 Ma) that outcropped in Hoh Xil, central Tibetan plateau. Based on theelectron microprobe analysis data, the xenoliths provide constraints for the formation equilibrium temperatures of the two-pyroxene gran-ulite being about 783 to 818℃ as determined by two-pyroxene thermometry and the forming pressure of the clinopyroxene granulite beingabout 0.845 to 0.858 GPa that is equivalent to 27.9～28.3 km depth respectively. It indicates that these granulite xenoliths represent thesamples from the middle part of the thickened Tibetan crust. This discovery is important and significant to making further discussion onthe component and thermal regime of the deep crust of the Tibetan plateau.     

Nd isotopic characteristics of Proterozoic metasedimentary rocks and constraints on their provenance in the eastern segment of Central Tianshan Belt, Xinjiang

Sm-Nd isotopic characteristics, εNd(t) values and Nd model ages (TDM) of Proterozoic metasedimentary rocks in the eastern segment of Central Tianshan Belt (ESCTB), Xinjiang, are used to constrain the sedimentary provenance as well as to evaluate their tectonic implications. εNd(t) and TDM values of these samples range from -4.00 to +6.36 and from 1.29 to 2.29 Ga, respectively. These feature values are distinguished from those of Archean Tarim Craton. Their average εNd(t) values of the Weiya, the Kumishi and the south to the Dikar samples are -2.46, +2.06 and +1.37, respectively. Nd model ages of the Weiya samples vary between 1.86 and 2.29 Ga, but those of the Kumishi and the south to the Dikar samples show a significant concentration at 1.6～1.9 Ga and the youngest Nd model age is 1.29 Ga. Those Nd isotopic characteristics suggest that these metasedimentary rocks could be derived from a significant proportion of Paleoproterozoic crustal source and a participation of young arc materials, rather than Archean Tarim Craton. Furthermore, the data also indicate that these two sources were paleogeographically separated. Thus we can deduce that the Kumishi and the south to the Dikar metasedimentary rocks were formed proximal to the arc side of the back-arc basin, but the Weiya metasedimentary rocks were closer to the continental side of the back-arc basin.     

Isotopic evolution of the terminal Neoproterozoic and early Cambrian carbon cycle on the northern Yangtze Platform, South China

Profound geotectonic, climatic and biological changes occur during the terminal Neoproterozoic and its transition into the early Cambrian. These are reflected in temporal variations of the chemical and isotopic composition of seawater. We are studying a sequence of sedimentary rocks at the Shatan section, northern Yangtze Platform, Sichuan Province of China. This succession comprises, in ascending stratigraphic order, predominantly calcareous sediments of the Sinian upper Dengying Formation and black shales of the lower Cambrian Guojiaba Formation (time equivalent of Niutitang Fm.). Paleoenvironmental setting represents shallow-water shelf deposits. The objective of our study is to provide temporal records for the isotopic compositions of organic and carbonate carbon throughout this time interval. Organic carbon isotope values display a range between -35.8‰ and -30.1‰ with clear stratigraphic variations. Carbonate carbon isotope data vary between -3.5‰ and +0.5‰. These secular variations are interpreted to reflect perturbations of the global carbon cycle, specifically changes in the fractional burial of organic carbon. However, local conditions have further affected the isotopic signals.     

熔融碳酸盐燃料电池阴极材料制备与导电性

研究了熔融碳酸盐燃料电池（MCFC）阴极材料锂铁氧化物电极的导电性能。实验结果表明在合成锂铁氧化物的过程中，使Li2CO3轻微过量，可以提高锂铁氧化物电极的导电性。在同一温度下，随着Li:Fe值的增大，锂铁氧化物电极的导电性增加。相同Li:Fe条件下，锂铁氧化物电极的导电性随着温度升高按指数规律增加。扫描电镜研究（SEM）表明，Li:Fe比值不同，制备的锂铁氧化物电极表面形貌也不同。     

某隧道围岩掉块成因分析

对某隧道为例，应用工程地质学，地质力学的方法对隧道围岩掉块的成因进行了分析，并对围岩的稳定性用赤平投影进行了解析，对围岩的稳定性判断提供了理论和实践依据，指出隧道中的不稳定块体主要为由于不良地质界面和临空面的相互组合形成的不稳定滑塌体。构造体系的型式为岩体的结构组合型式划分提供了依据，据此就可定性的评价岩体的稳定性，除此而外，隧道岩性及其组合，地应力及构造应力的大小和方向也是引起隧道围岩掉块不可忽视的因素。     

岩体复合型裂纹的扩展规律Ⅱ.有水作用条件下

基于最大周向正应力理论，研究并给出有水作用的复合型裂纹在不同应力状态及化学损伤作用下扩展的临界应力强度因子和扩展方向角。分析表明，裂纹水压力对不同受力状态复合裂纹的扩展规律的影响是不同的；化学损伤对岩体应力强度因子和裂纹扩展的方向具有很大影响。