略谈太平天国忠王府苏式彩绘

苏州太平天国忠王府现存四百余方梁枋苏式彩绘,这些彩绘内容多为传统吉庆题材,寓意吉祥祈福。众多木构件上的彩绘是明清以来苏式彩绘的典范,为明清时代所留而经太平天国利用改造而成;九幅壁画则是太平天国时期的作品,体现了太平天国壁画的艺术特色。忠王府苏式彩绘为研究明清苏式彩绘和太平天国彩绘提供了丰富的资料。     

论阿玛尔纳时代埃及与米坦尼的关系

阿玛尔纳时代早期,埃及和米坦尼都积极发展两国关系,将两国友好关系推到顶峰.阿玛尔纳时代后期,埃及面对中东错综复杂的局势,做出了疏远米坦尼的外交决策,而米坦尼面对赫梯的威胁,力图保持与埃及的友好关系,为此进行了不懈的努力.埃及与米坦尼关系的恶化对中东政治格局产生了深远影响.     

江苏省地理景观与美丽乡村建构研究

乡村审美空间蕴含着内在和深刻的人地关系理念内容,比经济效应有更深的自然情怀,是可持续发展的思想感情基础,也是现代景观规划的重要研究课题。城市化发展过程中自然地理脉络破坏对于乡村景观是致命的。探讨以多尺度层面的地理景观建构乡村审美空间:在区域大尺度范围内设计地理视域观赏空间;在镇域中尺度范围内将生态文明和社会经济发展要求安排在景观空间格局配置中;在乡村小尺度范围内造就素雅含蓄的村落景观。江苏省乡村具有四千年的历史,留下珍贵的人地关系文化遗产和审美烙印。从地理景观形态结构、格局演化进程与机理响应对照乡村审美空间景观,建构和谐安宁的画面境界;最终造就广阔地域的"美丽乡村"。     

THE EARLIEST USE OF CORUNDUM AND DIAMOND,IN PREHISTORIC CHINA*

The majority of prehistoric lithic artefacts were fashioned from rocks and minerals no harder than quartz, and there is no prehistoric evidence for the working of harder materials, such as corundum and diamond. The earliest physical evidence for the use of corundum (ruby, sapphire) is thought to be the abrasive grit recovered from Bronze Age Minoan quartz beads (c. 1700–1500 bc ), while diamond is thought to have been used no earlier than 500 bc , in India. Here we show that corundum was worked c. 4000–3500 bc during the Neolithic period in China, in the form of polished axes from the Liangzhu and Sanxingcun cultures. We also present physical evidence that later Liangzhu axes (c. 2500 bc ), made from the same previously undescribed rock whose most abundant component is corundum, were polished to a mirror‐like finish with a diamond abrasive. Our findings, which are the first to support the use of corundum and diamond in a prehistoric context, may also help to explain the trademark feature of the Neolithic in China, vast quantities of finely polished nephrite jade artefacts.     

《国语·晋语八》韦昭注辨正

本文以《国语·晋语》韦昭注为主要研究对象,在前贤时哲研究成果的基础上,揭出<晋语>中21处文本或韦注,认为其中有些是韦注本身的问题,前贤尚未发现;有些是前贤已经发现了的韦注的问题,但尚未给予真正解决;有些则是文献流传过程中出现的问题,虽未必与韦注有关,但涉及对《国语》的理解。本文逐一进行分析、解决。本文讨论《七录序》涉及的两个早期目录学史上的重要问题。《晋中经簿》在四部之外,又分为14卷,具有一定的二级分类意义。《古今书最》记载的图书存佚数字,是王俭而不是阮孝绪本人的统计结果。     

发展农业旅游略议

农业旅游作为一种富有特色、深受旅游者欢迎的新兴旅游业态,正越来越受到人们的关注。本文追溯了中外农业旅游发展的进程,分析了农业旅游发展的模式和特点,着重指出近年来我国的农业旅游迅速发展的主客观因素,并对如何开展农业旅游提出对策。     

景德镇早期青白瓷的器型与色度

早期青白瓷是学术界关注的热点之一。2006年发掘的铜锣山、道塘里窑址被认为是景德镇地区最早烧造青白瓷的窑业遗存。借助类型学和色度学方法,本研究对两窑出土早期青白瓷进行了系统分析和研究。结果表明,所谓的早期青白瓷,绝大多数更接近于定窑白瓷,而明显不同于典型的湖田窑青白瓷。研究为了解景德镇地区早期青白瓷的釉色特征、技术来源与发展脉络提供了重要的科学线索,为进一步研究景德镇早期青白瓷的缘起与演进奠定了基础。     

中国古代园林设计中的自然理想观

自然地理环境早先与现代都对人文传统的景观有很大影响。中国古代风景园林发源于自然生态环境的审美选择,进而以顺乎自然的设计指导思想求得"虽由人作,宛自天开"的审美标准,更有人与自然相与融洽的审美理想。西方古典园林中人造的几何规则景观超越于一切自然。在现代中国盲目模仿西方城市摩天大楼景观的时候,现代西方城市规划学者正致力于研究中国古代先哲的思想精髓和古代文化遗产,为塑造现代人居环境的自然协调寻找新的灵感启迪。     

南京城市沿长江段景观规划研究

南京城市滨江带具有山、水、城、林、洲相融合的特色环境,以往滨江地段功能的主要是工业生产和港口运输。目前科学地进行滨江景观规划强调沿江的生态和旅游功能,这对于南京市的进一步发展有重要意义。本文通过对历史时期南京城市滨江带功能演变的分析,深入滨江带景观现状调查和研究,对各个区域景观要素探讨,提出景观规划的指导思想与原则,并依此进行南京城市滨江带景观规划,划分为六个特色区域:河西滨江段,下关滨江段,幕燕滨江段,江中洲地段,大厂滨江段,浦口珠江段。     

Geophysical signatures associated with fluid flow and gas hydrate occurrence in a tectonically quiescent sequence,Qiongdongnan Basin,South China Sea

Interpretation of high‐resolution two‐dimensional (2D) and three‐dimensional (3D) seismic data collected in the Qiongdongnan Basin, South China Sea reveals the presence of polygonal faults, pockmarks, gas chimneys and slope failure in strata of Pliocene and younger age. The gas chimneys are characterized by low‐amplitude reflections, acoustic turbidity and low P‐wave velocity indicating fluid expulsion pathways. Coherence time slices show that the polygonal faults are restricted to sediments with moderate‐amplitude, continuous reflections. Gas hydrates are identified in seismic data by the presence of bottom simulating reflectors (BSRs), which have high amplitude, reverse polarity and are subparallel to seafloor. Mud diapirism and mounded structures have variable geometry and a great diversity regarding the origin of the fluid and the parent beds. The gas chimneys, mud diapirism, polygonal faults and a seismic facies‐change facilitate the upward migration of thermogenic fluids from underlying sediments. Fluids can be temporarily trapped below the gas hydrate stability zone, but fluid advection may cause gas hydrate dissociation and affect the thickness of gas hydrate zone. The fluid accumulation leads to the generation of excess pore fluids that release along faults, forming pockmarks and mud volcanoes on the seafloor. These features are indicators of fluid flow in a tectonically‐quiescent sequence, Qiongdongnan Basin. Geofluids (2010) 10 , 351–368