The discovery of early Permian reef belt in east Kunlun and its significance

The early permian reef belt is distributed in the southern side of eastern Kunlun, north area of Qinghai-Tibet Plateau. The core-reef facies of thc reel extends from Tuosuo Lake to Huashixia. Lots of reef breccia was found at the southern slope of the mre-reef belt, and to the north of the reef belt there is back-reef limestone. Cacisponges, hydrozoa, bryozoa,Tabulozoa, Tubiphytes and red algae are the main frame-building organisms.Archaeolithoporella, laminated blue-green algaes,Tabulozoa andTubiphytes played a role of binding or encrustating. There are many kinds of epibiont in the mf, including brachiopod, gasterid, foraminifera, echinoderm and simple coral. The type and the characteristics of the reef-building organisms in eastern Kunlun and Animaqing are basically thr same as those in the south of Chi     

Observational study of the circulation in the southern South China Sea

CTD data from two oceanographic survey cruises, conducted by “Shiyan No. 3” R/V during two reversing monsoons, were employed to calculate and analyze the distributions of temperature, salinity and geopotential anomaly in the southern South China Sea (SSCS). Based on these distributions, the horizontal structures of the SSCS circulation are described systematically. Study results show that the SSCS circulation structure could be classified as a two-layer (the upper and the lower) pattern, and that the main circulation in the upper layer (0–400 m) is driven by the South China Sea monsoons and is opposite in direction to the reversal of the monsoons. The distributions of principal current systems and their features are presented. Two important local phenomena, local eddy and oceanic front, were observed.     

Discovery of Permian island-arc basalts in the Cenxi area and the tectonic significance──A piece of evidence for the paleo-Tethyan tectonic belt in western Guangdong and eastern Guangxi

Cenxi Permian basalts are the late Palaeozoic island-arc type basalts first found in South China. REE and trace element characteristics and distribution patterns show that this volcanic formation, which has been isotopically dated at 261 MaB.P. by the 39Ar/ 40Ar method, is of an active continental marginal island arc type, and that the tectonic environment at that time was an island-arc marginal sea or minor ocean basin related with the paleo-Tethyan tectonic belt in western Guangdong-eastern Guangxi.     

南海夏季风活动激发的大气遥相关型

北半球夏季,南海地区是全球大气热状况变化最为激烈的区域之一,而南海夏季风则是该地区最为活跃的天气事件,它的演变必将导致其它地区大气环流的响应．通过相关计算、合成分析等手段,揭示与南海夏季风活动相关联的北半球大气遥相关型的存在．该波列状的遥相关型与东亚地区相连,经北太平洋延伸至北美西岸．最高的相关位于西太平洋副热带高压区域,因而它可能对我国旱涝天气产生重要影响．     

一个中国湿地植物资源分类系统

提出了一个中国湿地植物资源分类系统,并将我国湿地植物资源分为３大类２４小类,这个系统根据湿地植物用途建立系统框架,将植物群落的建群种,分布广的植物,生物量大的植物,湿地特有植物和与水禽,野生动物栖息地,繁殖地,隐蔽地相关的植物作为选择资源植物类别的标准。     

贺兰山苔藓植物物种多样性,生物量及生态学作用的研究

研究了贺兰山不同海拔高度主要林型种苔藓植物物种多样性,生物量和生态学作用,结果表明,云杉林下藓类地层的生物量最高,９１４７．７ｋｇ／ｈｍ＾２,是林灌木和草本植物总生物量的９．２倍,在饱和吸水状态下,可贮存水２０１７４．５ｋｇ／ｈｍ＾２,通过随机取样按海拔高度,林型和土壤类型等梯度对贺兰苔藓植物被进行了调查,影响苔藓植物生长和分布的主要生态因子是光照,相对湿度,海拔高度和土壤ｐＨ对出现在群落中包拓苔     

氧同位素：追踪陆架海沿岸水团变化的良好标志

对于陆架海而言除了冰体积效应,温度效应外,还有由于大陆淡水注入引起的,使δ＾１８Ｏ值负向偏移的效应,而且在低海平面时期,当沿岸水团盛行时,这种效应起主导作用。笔者将这种效应从广州的盐度效应中分离出来,称为陆架海的负值效应。     

论民国新儒家的政治合作化与现代化构建

民国新儒家认为政治现代化要通过合作化走和平建设之路,要先利用合作化帮助劳动阶级实现经济自助,培育和锻炼下层民众,再以合作化逐步改造资产阶级,调和阶级关系,最后以合作实现他们的理想政治王国。这是一个完整的政治构想,表达了儒家精神传统的济世情怀与对中国政治的国情思考,是西方合作文化在东方地域移植的必然结果。     

台风Utor登陆广东过程的数值研究

台风Utor(0104)于2001年7月6日00时(UTC,下同)在广东汕尾地区登陆,带来比较严重的灾害性天气.以美国国家大气研究中心和宾州大学联合研制的第五代中尺度模式(MM5)为基础设计的台风预报模式比较准确地预报出台风Utor(0104)的移动路径(前24 h的移动路径平均误差为 68 km)和天气现象的分布.在此基础上,设计了3个敏感性试验:①是把华南地区(26°N以南,110°E以东)的陆地变为海洋,②是把华南地区的山地变为平地,③是减小华南地区陆地的粗糙度,即取为近似于静风的洋面上的值.对比数值试验的结果表明:引起台风登陆后减弱的最主要因子是下垫面水汽供应的切断,其次是下垫面粗糙度(摩擦)的影响;地形作用能使迎风坡的降水明显增加,但对台风强度则没有明显的影响.     

论西藏经济环境特殊性与全面建设小康社会的联系

文章从跨越式发展和小康社会的内在联系入手，阐明了西藏在跨越式发展和全面建设小康社会的进程中，西藏经济环境的特殊性表现。剖析了西藏经济环境建设存在的诸多机遇与所取得的成就，从而阐述了我区在跨越式发展中全面建设小康社会的可行性。提出了在西藏实现跨越式发展，全面建设小康社会的市场环境建设的措施。