美丽总令人忧愁——沈从文“湘西人生形式”的审美意蕴

沈从文以“边城”为代表的湘西题材小说,表现了一种“优美、健康、自然而不悖乎人性的人生形式”,具有很高的审美价值。然而,湘西题材创作的审美意蕴,不仅表现这一人生理想上外化的生活、自为的性爱使这一形式获得了定性,而作家对湘西民族历经磨难的历史和生存危机的现实的感叹揉进这一人生形式中,更使作品获得了更耐人寻味的审美效果,达到了作家提出的“美丽总令人忧愁”这一审美境界。     

试论井冈山精神在高校思想政治工作中的开发与利用

井冈山精神是革命传统精神与时代精神的有机统一。当前,在高校思想政治工作中开发利用井冈山精神不仅可能,而且很有必要,十分重要。必须在科学把握井冈山精神实质的同时,依托高校党委的政治优势和健全的思想政治工作网络,坚持实事求是,与时俱进,不断创新思想政治工作的方式、方法和原则,提高思想政治工作的针对性和实效性。     

统筹城乡经济社会发展:解决“三农”问题的重大战略

统筹城乡经济社会发展是解决“三农”问题、实现城乡经济良性循环的必然选择;是解决“三农”问题的重大创新;是全面建设小康社会内在要求的深刻体现。我们要通过深化改革,改变城乡二元结构,建立平等和谐的城乡关系,推进城乡经济社会统筹发展。     

爱因斯坦和玻尔的科学创新方法论原则

本文在深入研究、比较爱因斯坦和玻尔科学创新方法及其特点的基础上,揭示了科学创新活动应当遵循的方法论原则,即哲学思想渗透原则、逻辑思维与非逻辑思维相结合原则和思想实验与物质实验相结合原则。     

浅谈对《中学体育与健康课程标准》的思考

《中学体育与健康课程标准》出台,中学体育教育从性质、价值定位等方面发生了很大变化,它要求教师从观念到教法均要与时俱进,但对在实施过程能否顺利推进,笔者提出了一些问题。     

加强物理方法教育的认识

从介绍物理基本方法入手,阐明物理方法教育的重要作用,强调在物理教学中必须加强物理方法教育.     

腐蚀管线的剩余寿命预测

预测管线的腐蚀变化趋势及腐蚀对管线结构完整性的危害是评价管线剩余寿命的关键步骤。将影响管线剩余寿命的各种因素看成是分布各异的随机变量 ,建立了预测管线失效的概率数学模型。利用这一模型 ,研究了腐蚀速率、缺陷深度、管道壁厚和工作压力等因素对管线可靠性的影响。结果表明 ,各参数的不确定性越大 ,管线的可靠性越低 ;缺陷深度在腐蚀缺陷形成初期 ,对管线的可靠性有很大影响 ,而随着时间的推移 ,腐蚀速率将对管线的可靠性有较大影响。对一条输油管线 ,基于管线腐蚀检测数据 ,对 1km长度的管道进行失效概率统计分析得到的腐蚀速率能够对管线全线的安全状况做出合理预测 ,从而为管线的进一步维修与检测提供参考资料。     

辽河盆地东部凹陷北部地区Es1+2/Es3不整合面与油气运聚的关系

根据 2 2 4口井的实际资料 ,结合地层沉积特征和地震剖面解释结果对辽河盆地东部凹陷北部地区Es1+ 2 /Es3 不整合面的上、下地层的接触关系及岩性组合特征进行了平面规划及分类 ,探讨了该不整合面与油气运聚的关系。研究结果表明 ,不整合面在油气运聚过程中所起的作用主要是由不整合面上、下地层的接触关系及岩性配置所决定。研究区凹陷北部茨 5 9井—茨 80井、龙 12井—龙 2 4井等区域为寻找不整合面之下遮挡油气藏的有利地区 ,茨 6 7—茨 6 15区域是该不整合面之上油气聚集的有利区     

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.