中国南方大地构造演化及其对油气的控制

按照板块构造理论及活动论、阶段论的思想，大致以中晚三叠世为界，将中国南方自震旦纪以来大地构造演化历史划分成海相盆地演化阶段（Z－T2）及陆相盆地演化阶级（T3－Q）两大阶段；又可进一步细分为扬子克拉通及其周缘裂谷盆地（Z－1q)、裂谷－克拉通－被动大陆边缘盆地（1c-O1）、被动陆缘－克拉通－前陆盆地（O2－S）、加里东运动（S末）、裂谷－克拉通盆地（D－T1）、克拉通残留海盆－弧后（浊积）盆地（T2）、印支运动（T2－T3）、华北－华南板块焊合、古特提斯封闭与前陆盆地的形成（T3－J2）、压扭背景下的改造作用及拉分盆地的形成（J3－K1）、伸展－裂陷盆地的形成（K2－E）、喜马拉雅运动（E末－N初）及披盖性构造层的形成（N－Q）12个阶段。特别是对南方自中晚三叠世以来的大地构造演化及其对现存油气的控制作用进行了系统研究，提出了晚侏罗世－早白垩世燕山运动对南方中生界、古生界原生油气藏的保存与破坏起到了决定性作用及燕山、喜马拉雅运动控制了现今南方原生、次生及再生烃（二次生烃）油气藏分布的新观点。     

B0型空间上共轭凸函数的指数共轭性

引入并刻划B0型准范空间中凸函数的上、下指数，建立共轭凸函数上、下指数间的完整共轭关系。     

TD—SCDMA系统定位算法研究与仿真

为了克服NLOS信号对移动无线电定位的影响，对TD－SCDMA系统中联合DOA与TOA实现移动终端定位的方案进行了研究，基于NLOS信号识别的算法有效地解决了NLOS信号对实施定位的影响，提出了一种对多基站时间加权定位算法，通过仿真实验证明了所采用算法的可行性，在NLOS情况下也可满足FCC对E－911业务的要求。     

视频会议系统中基于Mpeg4视频流的带宽控制

论述了一种基于Mpeg4数据流的速率控制解决方法 ,实现了应用在视频会议系统Admire中的视频网关VGW ,使系统在组播网络和单播网络互通的基础上 ,能够调整对单播用户 (可用带宽较低用户 )的视频发送速率 ,达到充分利用网络带宽和避免网络拥塞的目的     

A new species of Gobiconodon （Triconodonta, Mammalia） and its implication for the age of Jehol Biota

A new species of Gobiconodon is found from the Yixian Formation of western Liaonlng, China. The new taxa,G zofiae sp. nov., has a confluent opening for branches Ⅱand Ⅲ of the trigeminal nerve on the anterior lamina of the petrosal. G zofiae sp. nov. is similar to Repenomamus in having an ossified Meckel‘s cartilage connecting the lower jaws and ear region. The new species, with enlarged I^1/I1, posteriorly located infraorbital foramen and four mental foramina,distinctly differs from the other species of Gobiconodon. The new material indicates that Gobiconodon has four, not five,upper molariforms. The presence of Gobiconodon in Jchol Biota makes it possible to correlate Jehol Biota with faunas in eastern Asia and North America, and suggests the age of the Yixian Formation to be Early Cretaceous.     

A surface-based DNA algorithm for the minimal vertex cover problem

Abstract DNA computing was proposed for solving a class of intractable computational problems, of which the computing timewill grow exponentially with the problem size. Up to now, many achievements have been made to improve its performance and increase itsreliability. It has been shown many times that the surface-based DNA computing technique has very low error rate, but the technique hasnot been widely used in the DNA computing algorithms design. In this paper, a surface-based DNA computing algorithm for minimal ver-tex cover problem, a problem well-known for its exponential difficulty, is introduced. This work provides further evidence for the abilityof surface-based DNA computing in solving NP-complete problems.     

凝点附近含蜡原油的粘弹性研究

使用控制应力流变仪 ,在原油凝点附近温度区域对大庆原油和胜利原油进行了线性粘弹性应力范围内的小振幅振荡剪切实验。以原油开始出现线性粘弹性应力区间的最高温度作为基准温度定义了相对温度 ,对粘弹性参数进行了分析对比。研究表明 ,大庆原油及胜利原油在各自凝点以上 4℃时 ,均表现出明显的粘弹性特征 ,其损耗角分别为 37.6 6°和 76 .5 5°。在相同的相对温度下 ,大庆原油的弹性特征明显好于胜利原油 ,大庆原油的粘弹性参数对温度的敏感性也明显好于胜利原油。两种原油粘弹性不同的主要原因是其胶质、沥青质含量和析蜡特性不同。凝点温度附近的原油流变性及其随温度的变化规律应该作为确定输油管道进站温度的重要依据 ,目前 ,仅以原油凝点作为确定进站温度的主要依据是不合理的。     

HV/CVD Grown Relaxed SiGe Buffer Layers for SiGe HMOSFETs

High-vacuum/chemical-vapor deposition (HV/CVD) system was used to grow relaxed SiGe buffer layers on Si substrates. Several methods were then used to analyze the quality of the SiGe films. X-ray diffraction and Raman spectroscopy showed that the upper layer was almost fully relaxed. Second ion mass spectroscopy showed that the Ge compositions were step-graded. Transmission electron microscopy showed that the misfit dislocations were restrained to the graded SiGe layers. Tests of the electrical properties of tensile-strained Si on relaxed SiGe buffer layers showed that their transconductances were higher than that of Si devices. These results verify the high quality of the relaxed SiGe buffer layer. The calculated critical layer thicknesses of the graded Si1-xGex layer on Si substrate and a Si layer on the relaxed SiGe buffer layer agree well with experimental results.     

Mn∶Fe∶LiNbO3晶体两波耦合温度特性实验研究

本文对 30℃至 1 2 0℃温度范围内的光折变晶体Mn∶Fe∶LiNbO3的前向双光束耦合的温度特性进行了实验研究 .发现在 5 0℃、70℃和 1 0 5℃附近出现异常峰值 .     

Holocene lake deposits of Bosten Lake, southern Xinjiang, China

A 9.25-m-long sediment core from Bosten Lake,Xinjiang, provides detailed information about changes in the water budget and biological acticity over the last 8400 cal-endar years. The chronology is constructed from six AMS radiocarbon dates on the terrestrial plant remains. Based onanalyses of TOC, CO3, detrital compounds and biogenic SiO2,lake level fluctuations and periods of remarkably-negative water budget appeared at 8.4-8.2 cal ka, 7.38-7.25 cal ka,5.7-5.5 cal ka, 3.7-3.4 cal ka and 3.3-2.9 cal ka, respec-tively. As they are in-phase with low lake levels at Sumxl Co and Bangong Co in western Tibet Plateau and with paleo-lakes in Inner Mongolia, a climate-induced change to some-what drier and warmer conditions is inferred. A further drop in lake level after 1320 AD of about 200 yr duration may heattributed to a negative water balance prior to the main phase of the Little Ice Age. Deep and stable lake phases of 1500 yr and 1800 yr duration at 7.2-5.7 cal ka and 5.5-3.7cal ka coincide with maximum moisture during the Holocene Megathermai in China. The long term trend towards aridity since about 4.3 cal ka can dearly be recognised. The reduced water budget of Bosten Lake from 640-1200 AD may be attributed to local effects.