嵩山夷平面研究

夷平面研究作为一个永远年轻的课题,在经过1890～1910年和1950～1970年两次研究高潮以后,目前再度成为国内外地学界研究的热点,正在酝酿着第三次研究高潮.本文在形态分析、构造分析和相关沉积分析的基础上,确定了嵩山山顶古平坦面是早第三纪晚期形成的夷平面,它可与华北以及全球陆地同期的地形面进行对比.     

白沙县黎族贫困山区中学生参加课外体育活动的动机调查与分析

通过实地考察、问卷调查、文献资料、座谈和统计,对白沙县黎族贫困山区中学生参加课外体育活动的情况进行调查,结果显示白沙县黎族贫困山区中学生参加课外体育活动的动机主要是为了提高学习效率、丰富生活情趣、增强体质,兴趣趋向集中于健身性、健美性、趣味性、娱乐性和竞技性.     

高校内部MIS的集成与信息交换

简要介绍了高校内部MIS的现状；指出异构数据库是客观存在的历史问题，认为如何实现异构数据库之间的透明访问是信息交换和系统集成的关键；总结了异构数据库互操作的常用方法以及它们的工作原理，并提出了一种基于XML的解决方案。     

对北京地区中学物理教师教科研能力的调研

根据对北京市中学物理教师教育科研能力现状的调查，分析了目前中学物理教师的教育科研能力现状与造成这种现状的原因，并对怎样提高中学物理教师的教育科研能力提出了一些建议。     

常州市中学女生体育活动现状的调查与分析

本采用问卷调查等研究方法，对常州市中学女生的体育活动现状进行了调查分析，结果表明：多数女生喜欢体育课，且动机良好；对体育运动项目选择广泛；课外参加锻炼情况一般；学生自我锻炼意识差；掌握的体育理论知识与自我锻炼的方法较少。     

藏南特提斯晚三叠世海岸风成沙丘的发现及其意义

通过近年来的研究,首次在聂拉木县土隆村上三叠统德日荣组中发现了海岸风成沙丘沉积。其风成证据有:(1)普遍具风成大型交错层理,倾角达20°～30°且倾向均一,交错纹层向上变薄,具反粒序,与下伏界面相切,层间界面多为高波痕指数(>15)波状风蚀起伏面。(2)见沙丘夹丘间沉积的基本层序。沙丘沉积单层厚2～6m,呈块状,结构松散。丘间沉积较薄,有时为透镜体,多为水道沉积,有些为具反粒序的风成沙席沉积。(3)沙丘砂由分选、磨圆好的石英砂组成,含量大于95%,具单众数粒度分布,无悬移质。(4)见角砾化前积层、牵引褶曲、倒转褶曲等常见的风成沙丘同沉积变形构造。(5)具有与水成砂岩完全不同的胶结特征。海岸风成沙丘的存在准确地标定了特提斯南岸的古海岸线位置、丰富了研究区的沉积类型,无疑对特提斯海的层序划分、海平面变化及其古地理演化研究具有一定意义。     

对开发性移民的法律解释

开发性移民方针的提出是我国水库移民理论的一次重大创新，开发性移民是对补偿性移民的发展．从法律角度来看，开发性移民的实质是遵循市场经济的基本规律，运用法制手段，以移民补偿和库区开发为基础，对国家、集体、个人利益关系的一种平衡和协调，以实现库区经济社会的可持续发展．     

A new Euprox from the Late Miocene of Yuanmou,Yunnan Province,China,with interpretation of its paleoenvironment

The Yuanmou Basin of Yunnan Province is a hotspot for the research of early homind evolution and its environmental background.During the implementation of the Program“Research of the Origin and Evolution of Early Man and Its Environmental Baqckground” from 1998 to 2001,a huge quantity of hominoid and mammal fossils were collected.The present report systematically describes an Euprox robustus sp.nov.identified during the recent laboratory work on the collected material.Euprox is a group of earliest cervids with true antlers.The new species is the third one of the genus discovered in China.Judged by its morphologic characteristics,the new species feed on juicy and tender leaves of dicotyledon.It implies that the vegetation of its epoch in the Yuanmou Basin is a kind of southern subtropical evergreen forest and the climate is humid and temperate with evident seasonality.The latter is mostly influenced by the monsoon and secondly by the latitude.     

Microstructure and functional morphology of the Early Cambrian problematical fossil Rhombocorniculum

Rhombocorniculum cancellatum from the Lower Cambrian of southern Shaanxi Province (South China) is represented by the dextral and sinistral tooth-like sclerites (both in nearly equal numbers), indicating that the body plan of the organism with these sclerites probably was bilaterian. The main feature of the microstructure of the sclerites is the presence of longitudinally arranged, mutually contiguous hollow tubules, the shared walls consisting of microcrystalline apatite. In transverse cross sections, the sclerite wall mainly exhibits a spongy structure, with pore size decreasing adapically. Functional morphological analysis indicates that the sclerites serve as a defensive rather than a grasping function.     

Early Cambrian eodiscoid trilobites of the Yangtze Platform and their stratigraphic implications

Analysis of the taxonomy and stratigraphic distribution of the Early Cambrian eodiscoid trilobites of the Yangtze Platform indicates that species of Tsunyidiscus and Hupeidiscus can be used for biostratigraphic correlation. T. aclis occurs only in the lower Qiongzhusian, T. armatus occurs in the lower and middle Qiongzhusian, while T. niutitangensis and T. tingi occur mainly in the middle and upper Qiongzhusian, with only T. tingi extending upward into the lower Canglangpuian. H. orientalis first appears in the upper Qiongzhusian, reaching peak abundance in the lower Canglangpuian and becoming extinct above the Drepanuroides Zone. Biostratigraphic and lithostratigraphic correlations indicate that the limestone in the lower part of the Mingxinsi Formation, the Upper Member of Jiumenchong Formation, and the upper part of the Middle Member of the Huangbailing Formation, can be correlated with each other as Hupediscus, an index fossil of the lower Canglangpuian, is abundant in all these units. The lower part of the Niutitang and Jiumenchong formations in eastern Guizhou, which mainly represent Qiongzhusian strata, can be correlated with the Lower Member of the Huangbailing Formation. The basal part of the Niutitang Formation, which may be equivalent to the Upper Meishucunian Shiyantou Formation in eastern Yunnan, is very condensed. Well-preserved sponge faunas and non-mineralized fossils in the lower part of the Niutitang and Hetang formations are not older than Qiongzhusian in age.