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。     

民族区域自治与西藏繁荣进步--纪念西藏自治区成立40周年

民族区域自治作为我党解决民族问题的基本制度，它在西藏的建立与实践，不仅巩固和发展了“平等、团结、互助”的社会主义民族关系，而且促进了西藏经济、文化等事业的全面繁荣进步。四十年的实践证明，这一制度既符合中国的国情，也符合西藏的区情。     

西藏日喀则地区恰布林组物源分析

长期以来，沿西藏雅鲁藏布江南岸呈东西向展布的恰布林组砾岩，被认为是造山期后磨拉石的产物，而被置于第三纪。由于在屯穷紫色泥岩底部灰绿色粉砂质灰岩中发现腹足类化石Ｋａｔｏｓｉｒａｓｐ．，并结合其他地质证据，可以确定该组时代属于早中侏罗世。结合岩石学特征、典型砾岩中砾石的岩石地球化学和物源区分析表明，恰布林组砾岩的砾石有相当一部分来自蛇绿岩，其特征明显不同于现今的雅鲁藏布江蛇绿岩。因此认为雅鲁藏布江存在早中侏罗世之前的古蛇绿岩。     

藏蒙汉宗教文化的相互交流及影响

藏传佛教文化渊源于汉地大乘佛教和南亚密教，在与土著本教几经较量后，形成独具一格的藏传佛教文化。由于自身的生命力和历史的政治风云影响，藏传佛教文化北扩、南下、东返，藏蒙汉文化交流融合历经千余年，使藏文化成为中华民族文化大家庭中不可分割的一部分。     

层次分析法在西藏日土地区旅游资源评价中的应用

旅游资源评价是科学开发旅游资源的基础.以西藏日土地区为例,运用层次分析法对其旅游资源进行评价,在系统分析基础上建立综合评价模型,经一致性检验后计算各因子的相对权值并模糊打分.结合权值结果和得分,分析了旅游品质、主次因子和旅游潜力.评价结果表明,日土地区旅游品质较高,在生态容量和环境容量框架内系统有序地开发当地旅游资源现实可行.为进一步开发日土地区旅游资源提供了可行性论证和参考措施.     

西藏阿里地区夏康坚雪山构造地貌特征及其形成机制

简述了冈底斯构造带夏康坚地垒断块山的组成及基本构造特征.根据该地垒两侧冰碛阶地的发育特征及ESR测年结果,可推断该地垒的主要形成期是中更新世.夏康坚地垒断块山的成因是在白垩纪早期的古隆起基础上,东西向断层的右行剪切走滑和隆升活动的联合作用下而形成.     

西藏措勤地区的下白垩统岩石地层单位评述

西藏区域地质调查大队在1:100万日喀则幅区调中将措勘地区划分为两个地层小区,各自建立了下白垩统的岩石地层系统.作者根据在该区测制的下白垩统连续地层剖面及相关地质调查,认为这两个地层小区并不存在;建议在措勤地区建立统一的下白垩统岩石地层系统,从下至上划分为则弄组、多尼组和郎山组.     

西藏农村人力资本投资困境分析

农村人口综合素质整体不高,日益成为西藏农村反贫困和可持续发展的重要制约因素之一,加大人力资本投资日益迫切.文章提出没有基于本地化的农村办学思路,师资队伍整体落后与教育质量不高长期并存,教育投资观念偏差根深蒂固,基层卫生服务能力薄弱及健康知识普及严重不足等是当前西藏农村人力资本投资存在的诸多困境,并指出尽快优化教育发展结构、突出师资队伍建设、加强成人培训力度、关注妇女儿童健康是提高农村人口发展能力的重要途径.     

A high-resolution environmental change record since 19 cal ka BP in Pumoyum Co,southern Tibet

A 380-cm-long sediment core was acquired from the deep water area of Pumoyum Co, southern Tibet. Twenty-five plant residue samples were selected, and organic carbon stable isotopes were obtained using the AMS ¹⁴C chronological method. The ¹⁴C age and carbon reservoir effect were calibrated with surface sedimentation rate measurements using ²¹⁰Pb dating. Results showed that the core sediment deposited over 19 cal ka BP. Based on a multi-proxy analysis of TOC and IC contents, grain size and pollen assemblage data, the palaeoclimatic evolution of Pumoyum Co was reconstructed since the last glacial. Pumoyum Co was a shallow lake prior to 16.2 cal ka BP; although the glacier around the lake began to melt due to increasing temperatures, climate was still cold and dry. In the interval of 16.2–11.8 cal ka BP, the sedimentary environment fluctuated drastically and frequently. Two cold-events occurred at 14.2 and 11.8 cal ka BP, and these may correspond to the Older Dryas and the Younger Dryas events, respectively. After 11.8 cal ka BP, Pumoyun Co developed into the deep lake as it is now. The lake water temperature was relatively lower at that time because of influx of cold water from glacial meltwater entering the lake. As a result, the multi-proxy indicators showed no sign of warm conditions. Comparisons between the sedimentary record of Pumoyum Co with that of other lakes of the same age in southern Tibet indicate a warmer climate following the last deglaciation influenced the southeastern Tibetan Plateau. These results imply that the southwest Asian monsoon gradually became stronger since the deglaciation during its expansion to the inner plateau. The glacial-supplied water of the lake responded sensitively to cold-events. The entire southern Tibet region was dominantly influenced climatically by the southwest Asian monsoon during the Holocene.