铜鼓是东盟古代文化的共同载体

铜鼓广泛分布于中国南方和与之相邻的越南、老挝、柬埔寨、缅甸、泰国及马来西亚和印度尼西亚等东南亚国家。铜鼓是这些国家和民族在两千多年的漫长历史中,通过各种形式的交往与融合形成的共同文化载体。     

中国西部城镇化发展的“三分”构想

在经济全球一体化和经济区域化已成为当今世界经济发展大势的背景下，西部区域经济之所以发展不利，根本原因是区域经济理论陈旧落后，缺乏创新的区域发展思维。这些深层次的问题得不到解决，西部的城镇化水平和区域经济难以得到快速发展。因此，“三分构想”的提出是十分必要和迫切的。     

The Generalized West Decomposition of Operators and Other Compact Perturbation Problems

This paper introduces the concept of the generalized Riesz operators and the concept of the generalized West decomposition of a general operator which generalizes the definition of the West decomposition of Riesz operators, and proves that the following three statements are equivalent on a general Banach space： （a） Every generalized Riesz operator has the generalized West decomposition; （b） Every operator makes strong Stampfli theorem true; Every operator has Apostol＇s compact correction.     

以中日韩自由贸易区为核心和先导的东北亚合作模式

2003年10月中日韩三国领导人在印尼巴厘岛《中日韩推进三方合作联合宣言》的签署之后，东北亚合作的问题日益成为人们关注的焦点，加强东北亚各国的合作不仅有利于促进亚太区域内各国经济的发展，促成亚太地区经济进一步崛起，还会化解东北亚各国之间的矛盾和冲突．东北亚的合作应当加强信任、走制度化的合作道路，创设以中日韩自由贸易区为核心和先导的东北亚合作模式．以次区域合作先行的模式来带动东北亚经济一体化的发展。     

西秦岭南带中志留统的岩石学特征与沉积环境

详细研究了西秦岭南带中志留统岩石学特征,对遭受重结晶作用的碳酸盐岩进行了结构成因分类。分析了该区中志留世的沉积环境及变化特征。在该区发现的层孔虫生物礁及其它“浅水”标志,表明志留纪时,为若尔盖微古陆北侧的边缘浅海环境。西部为局限陆棚环境,可分为:局限内陆棚、海湾、礁滩-泻湖-潮坪(孤立台地)等亚环境;东部为开阔陆棚环境,可分为浅海砂滩、内陆棚、外陆棚等亚环境。     

西印度蔗螟聚集信息素次要组份合成方法的改进

2-甲基-4-庚醇和2-甲基-4-辛醇是西印度蔗螟(Metamasiushemipterus)聚集信息素的次要组份，本文以天然产物(S)-亮氨酸为原料合成出了2-甲基-4-庚醇及2-甲基-4-辛醇的所有对映异构体，其关键步骤是由(2S)-4-甲基-1,2-戊二醇合成出(2S)和(2R)-4-甲基-1,2-环氧戊烷两种重要中间体，目标产物光学纯度可达95%以上。     

CLIMATIC CHANGE SINCE LITTLE ICE AGE RECORDED BY DUNDE ICE CAP

The climatic change since the Little Ice Age recorded in the Dunde Ice Cap is presentedin this paper. There have been three cold periods and three warm periods since 1400AD.Among them, the coldest one was in the 17th century. Many evidences verified the three coldand warm variations recorded in the Dundc Ice Cap. But it was found from the comparison between the Dunde Icc Cap climatic record and thewinter temperature record in Shanghai that there was a temporal dfference in climatic changebetween East China and West China. The general trend is that the cooling and warmingprocesses in West China were earlier than that in East China. In the Dunde Ice Cap, it isnow in an anomalous warm period, while it is not as warm as in Dunde Ice Cap recordaccording to the winter temperature in Shanghai. In addition to the possible cause of temporaldifference in climatic change between West China and East China, another possible cause isthat the greenhouse effect of CO_2 may already be recognizable in the Dunde Ice Cap a     

Isocyanide addition to MN2(CO)5(Ph2PCH2PPh2)2 and the formation of a four-electron doubly-bridging isocyanide

The reactions of Fe(CO)₅, Fe(CO)₄P(C₆H₅)₃, M(CO)₆ (M  W, Mo, Cr), and (CH₃C₅H₄Mn(CO)₃ with KH and several boron and aluminium hydrides were investigated. Iron pentacarbonyl was converted quantitatively to K⁺Fe(CO)₄-(CHO) by hydride transfer from KBH(OCH₃)₃ allowing isolation of [P(C₆H₅)₃]₂-Nⁿ⁺Fe(CO)₄(CHO)^? in 50% yield. Lower yields were obtained with LiBH(C₂H₅)₃, and other hydride sources gave little or no formyl product. The stability of Fe(CO)₄(CHO)^? in THP was found to depend on the cation, decreasing in the order [P(C₆H₅)₃]₂N⁺ > K⁺ > Na⁺ > Li⁺. No formyl complexes were isolated and no spectroscopic evidence for formyl formation was observed in the reactions of the other transition metal carbonyls with several hydride sources. Fe(CO)₄-P(C₆H₅)₃ gave K₂Fe(CO)₄ when treated with KHB(OCH₃)₃. When treated with LiBH(C₂H₅)₃, W(CO)₆ gave a mixture of HW₂(CO)₁₀^?and (OC)₅W(COC₂H₅)^?; the latter was methylated to give the carbene complex (OC)₅WC(OCH₃)C₂H₅.     

The formation of a series of barium tungsten bronzes

The phases occurring in samples of gross composition Ba_xWO₃ (0.01 < x < 0.33) heated at temperatures between 1073 and 1373°K have been determined using X-ray diffraction and electron microscopy. At all temperatures a tetragonal tungsten bronze phase with a narrow homogeneity range of x = 0.20?0.21 was observed to form. In addition, at temperatures up to 1273°K, a series of orthorhombic intergrowth bronzes forms within a restricted composition range around x = 0.04. The latter phases are unstable at higher temperatures and were not found in preparations made at 1323°K. Similarly a new type of bronze phase forms at x = 0.14?0.16 at temperatures up to 1323°K, but not at 1373°K. The structure of this phase is unknown. Aspects of the crystal chemistry of the barium bronzes and the relationships to other bronze phases are discussed.     

Resonances with the complex rotation method: a study of an exactly soluble two-channel model

The complex rotation method is applied to the determination of widths and shifts of an harmonic oscillator predissociated by a linear potential, for when exact analytical formulas are available in the limit of small interchannel coupling. Excellent agreement is obtained.