Reconstruction of Early-Middle Jurassic Large Ordos Basin and Tectonic Setting

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A Model-Based Approach to Semi-Automated Reconstruction of Buildings from Aerial Images

Automated reconstruction of building objects from aerial images is a complex problem due to the diversity of buildings as well as noise and low contrast of images, which are the results of distant photography, atmospheric effects and poor illumination. In this paper, a semi-automated approach to the reconstruction of parametric building models from aerial images is presented, which works with line segments extracted from the image. The model is selected interactively from a library of parametric models. A perceptual grouping technique is used to select the most significant image lines in terms of relations such as proximity and parallelism. Model lines are searched for the same relations as in the grouped image lines, and the corresponding lines undergo a matching procedure, which determines whether or not a match can be found between the given model and image lines. An experiment with aerial images of flat-roof and gable-roof buildings is shown and its results indicate the robustness and efficiency of the proposed approach.     

泰安基准台洞体及环境改造

大部分形变仪器长年工作在山洞内,洞室的潮湿对仪器及房间内装修材料影响很大,“十五”期间中国地震局投资近十万元对泰安台形变仪器专用山洞进行了改造。本文从改造内容,改造方法及改造效果几方面进行了阐述,为同类山洞改造提供借鉴。     

数字技术力量下的乡村重构

随着数字技术逐渐深入到乡村生产生活的各个方面,乡村社会关系及空间意义发生重构。信息化冲击下的乡村空间转变不仅体现在物质方面,其社会文化空间意义及人地关系地域系统的重构在内生逻辑上重塑乡村话语权力和主体身份。论文通过探讨数字技术与乡村发展的多维关系及其对乡村产生的多重效应,关注数字技术带来的自由与异化、数字经济引发的话语与权力流变及乡村女性主体地位和身份的重构,解释了数字技术作为非人类行动者的主体性及其建构下的乡村日常经济生活和社会关系,拟为乡村性的分析框架提供有益的补充,为数字乡村建设和乡村振兴提供新的理论借鉴。     

对古地理再造中古地磁方法的回顾与探讨

古地磁数据的获取和应用是进行古地理再造的重要基础.同时,计算机技术的发展以及GIS技术的推广,极大地推动了古地理再造方法的革新,为古地理再造提供了更加方便、高效的软件辅助平台.本文主要围绕古地磁数据资料、应用方法及软件开发等方面,对其发展历史与研究现状作一详细的回顾与探讨.     

延庆地震台地电阻率改造影响的分析研究

对延庆地震台地电阻率的观测系统进行改造后的变化特征进行了初步研究,介绍了电极和外线路改造技术环节,并通过改造前后观测资料的对比分析对改造后的观测系统情况进行了评价。     

Research activities on land-use/cover change in the past ten years in China using space technology

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利用海洋温度剖面与海表盐度反演盐度剖面方法研究

为解决海洋中大量观测数据只含有温度剖面而缺乏盐度观测的问题, 基于历史观测的温盐剖面资料, 考虑到盐度卫星数据的发展, 采用回归分析方法, 在孟加拉湾建立了盐度与温度、经纬度、表层盐度的关系, 并对不同反演方法的反演结果进行检验评估。结果发现, 在不引入海表盐度(sea surface salinity, SSS)时, 最佳反演模型是温度、温度的二次项与经纬度确定的回归模型, 而SSS的引入则可以进一步优化反演结果。将反演结果与观测结果进行对比, 显示用反演的盐度剖面计算的比容海面高度误差超过2cm, 而引入SSS后的误差低于1.5cm。SSS的引入能够较为真实地反映海洋盐度场的垂直结构和内部变化特征, 既能够捕捉到对上混合层有重要影响的SSS信号, 又能够反映盐度在跃层上的季节内变化以及盐度障碍层的季节变化。水团分析显示, 与气候态相比, 盐度反演结果可以更好地表征海洋上层水团的变化特征。     

1959-2003年青海省干湿变化分析

利用青海省1959-2003年气象资料,计算了修正的Palmer干旱指数,并对其进行了分析。结果表明：在青海省旱涝监测中,PDSI指数反映旱涝程度更为客观;青海省的干旱主要以轻旱为主;夏秋季年际干湿交替较冬春季频繁,变化振幅也较大;秋季青海省干旱化倾向最为严重,冬春季出现轻旱几率最大。另外,春季干旱总面积在减小;夏季轻旱面积增加,而中旱、重旱面积在减小;秋冬季重旱面积在增加。     

Radiating 1.0 Ga Mafic Dyke Swarms of Eastern Brazil and Western Africa: Evidence of Post-Assembly Extension in the Rodinia Supercontinent?

Several mafic dyke swarms of similar composition and age (tholeiite- ca.1.0 Ga) occur on both sides of the Atlantic Ocean in eastern South America and western Africa. When assembled to their pre-drift position in the Mesozoic, the Brazilian coastal dyke province of Bahia, and the African dykes in Cameroun (Ebolowa suite) and Congo (Comba and Sembe-Ouesso provinces) define a giant radiating pattern (1200 km × 800 km) similar to other dyke swarms elsewhere associated with large-scale continental rifting. Magma flow indicators of the Brazilian dykes and branching propagation styles of their African counterparts indicate that the dyke conduits were fed with magmas diverging from a source beneath the long axis of the Meso-Neoproterozoic West-Congolian Basin in Africa. There, MORB-like metabasalts have been described in the La Bikossi Group of the Mayombian Supergroup. Whether the rifting event and intrusion of dyke swarms were triggered or not by a mantle plume beneath part of the Rodinia subcontinental lithosphere remain to be confirmed.