空间信息网格中远程空间连接查询的优化     

谢传节  刘高焕  高秉博  盛文涛 《遥感学报》2008,12(5)

随着空间信息网格的建设,网格平台上管理的空间信息资源越来越丰富,这促进了空间信息网格中空间数据分布式查询的应用需求,而在分布式空间查询中,空间连接查询操作往往成为性能的瓶颈.根据空间信息的特点,通过利用网格计算资源来优化空间连接查询的执行.首先基于网格服务构建网格平台分布式空间数据查询软件结构,通过设计远程空间连接执行服务利用网格平台中的计算资源;根据空间信息的特点.采用基于Kd-Tree空间分区并行连接的方法提高远程空间数据连接操作执行效率,并给出了远程空间连接执行的查询代价模型;然后根据连接代价模型设计了远程空间连接查询执行计划优化生成算法;最后总结了本文工作并探讨了下一步研究方向.  相似文献   

第四纪环境重建的良好代用指标——有壳变形虫记录与古生态学研究进展   总被引：2，自引：0，他引：2  

秦养民  谢树成  顾延生  王军霞  周修高 《地球科学进展》2008,23(8):803-812

有壳变形虫是一类广泛分布在淡水潮湿环境中的根足纲原生动物,具有较窄的生态幅、较短的生命周期,对环境变化敏感等特点,因此沉积物中保存的有壳变形虫化石可以提供高分辨率的环境信息。有壳变形虫化石在古湖泊学与人类活动、古水文、古温度、第四纪海平面变化的定量重建等方面具有独特而重要的研究价值。在欧洲和北美开展的大量研究已证实有壳变形虫是古环境变化的有效指示器。我国地域辽阔,生境多样,无论是开展现代有壳变形虫的生态学研究,还是沉积物中有壳变形虫记录的古环境重建,都有巨大的研究潜力。  相似文献   

GPS在计算导弹脱靶量中的应用研究     

周立锋  马斌  谢志博 《全球定位系统》2008,33(6):33-36

将GPS技术应用于导弹靶试脱靶量测量,并对计算过程作了较为详细的分析和探讨。试验证明：利用GPS测定脱靶量,测量精度高,简单易行,可以在靶场逐步试验推广。  相似文献   

吐哈盆地丘东凝析气藏中侏罗统储层流动单元划分     

解伟  马广明  孙卫 《现代地质》2008,22(1):81-85

对吐哈盆地丘东凝析气藏中侏罗统储层的流动单元的划分方法和参数选取进行探讨。针对丘东凝析低渗透气藏的储层和流体特点,纵向上对研究区中侏罗统地层进行小层精细划分,平面上应用SPSS统计分析软件对厚度、孔隙度、泥质含量、流动带指数等4个参数进行聚类分析和判别分析,将研究区中侏罗统储层砂体划分为4类流动单元。结果表明各流动单元的类型与储层物性、沉积微相具有很好的对应关系,能够客观地反映气藏储层的地质特征。虽然丘东凝析低渗透气藏中流动单元的划分和油藏中流动单元的划分没有太大差别,但是参数的选取却与油藏中的存在着明显的不同。  相似文献   

甘肃两河口地区水系沉积物异常评价   总被引：2，自引：0，他引：2  

苟建德  朱从龙  谢洪春  景煜瑧 《物探与化探》2008,32(2):135-138

对两河口地区1:5万水系沉积物资料处理,圈定了大量元素异常。应用R型因子分析结果,划分元素组合。从元素组合特征方面分析,评价异常找矿意义,确定了7个找矿远景区,其中1号异常为最佳找矿靶区。  相似文献   

南京市大比例尺地形图的动态更新和维护研究   总被引：1，自引：0，他引：1  

谢士杰 《测绘通报》2008,(1):46-49

城市规划需要现势性强的全覆盖的城市大比例尺地形图,城市规划、建设导致地形图的快速变化。如何处理这一对矛盾,最大程度地实现测绘对城市规划、建设和管理的保障,是一个难题。将测绘与规划管理的日常业务进行结合,提出一整套城市大比例尺地形图的动态更新和维护的方法,制定相应的数据标准和规范,研制了支撑平台,并在浦口区进行实践,具有较强的可操作性。  相似文献   

Geochemical Mapping: With Special Emphasis on Analytical Requirements     

XIE Xuejing  CHENG Hangxin  LIU Dawen 《《地质学报》英文版》2008,82(2):451-462

More than 40 national and regional geochemical mapping projects in the world carried out from 1973 to 1988 do not conform to common standards. In particular they have many analytical deficiencies. In the period 1988 to 1992, the International Geochemical Mapping project （Project 259 of UNESCO＇s IGCP Program） prepared recommendations designed to standardize geochemical mapping methods. The analytical requirements are an essential component of the overall recommendations. They included the following： 71 elements should be analyzed in future mapping projects; the detection limits of trace and ultratrace elements must be lower than the corresponding crustal abundances; and the Chinese GSD and Canadian STSD standard sample series should be used for the correlation of global data. A proposal was also made to collect 5000 composite samples, at very low sampling densities to cover the whole Earth＇s land surface. In 1997 an IUGS Working Group on Global Geochemical Baselines was formed to continue the work which began with IGCP 259. From 1997 up to now, new progress has been made especially in China and FOREGS countries under the aegis of this working group, including the study of suitable sampling media, development of a multi-element analytical system, new proficiency test for selection of competent laboratories and role of wide-spaced mapping in mineral exploration. One of the major problems awaiting solution has been the inability of many laboratories to meet the IGCP recommendations to generate high quality geochemical maps. Fortunately several laboratories in China and Europe have demonstrated an ability to meet the requirements and they will be well placed to render technical assistance to other countries.  相似文献   

Jurassic Tectonics of North China: A Synthetic View   总被引：21，自引：1，他引：20  

ZHANG Yueqiao  DONG Shuwen  ZHAO Yue  ZHANG Tian 《《地质学报》英文版》2008,82(2):310-326

This paper gives a synthetic view on the Jurassic tectonics of North China, with an attempt to propose a framework for the stepwise tectonic evolution history. Jurassic sedimentation, deformation and magmatism in North China have been divided into three stages. The earliest Jurassic is marked by a period of magmatism quiescence （in 205-190 Ma） and regional uplift, which are considered to be the continuation of the “Indosinian movement” characterized by continent-continent collision between the North and South China blocks. The Early to Middle Jurassic （in 190-170 Ma） was predominated by weak lithospheric extension expressed by mantle-derived plutonism and volcanism along the Yanshan belt and alongside the Tan-Lu fault zone, normal faulting and graben formation along the Yinshan- Yanshan tectonic belt, depression and resuming of coal-bearing sedimentation in vast regions of the North China block （NCB）. The Middle to Late Jurassic stage started at 165y.5 Ma and ended up before 136 Ma; it was dominated by intensive intraplate deformation resulting from multi-directional compressions. Two major deformation events have been identified. One is marked by stratigraphic unconformity beneath the thick Upper Jurassic molasic series in the foreland zones of the western Ordos thrust-fold belt and along the Yinshan-Yanshan belt; it was predated 160 Ma. The other one is indicated by stratigraphic unconformity at the base of the Lower Cretaceous and predated 135 Ma. During this last stage, two latitudinal tectonic belts, the Yinshan-Yanshan belt in the north and the Qinling-Dabie belt in the south, and the western margin of the Ordos basin were all activated by thrusting; the NCB itself was deformed by the NE to NNE-trending structural system involving thrusting, associated folding and sinistral strike-slip faulting, which were spatially partitioned. Foliated S-type granitic plutons aged 160-150 Ma were massively emplaced in the Jiao-Liao massif east of the Tan-Lu fault zone and indicate important crustal thicken  相似文献   

Distribution of Palygorskite in the Lingtai Profile of Chinese Loess Plateau: Its Paleoclimatic Implications     

XIE Qiaoqin  CHEN Tianhu  Chen Jun  Ji Junfeng  XU Huifang  XU Xiaochun 《《地质学报》英文版》2008,82(5):967-974

Palygorskite is a typical indicator mineral of the arid and strong evaporation environment. Distribution of palygorskite in loess-red clay sequences may act as an important indicator for reconstruction of the paleoenvironment and paleoclimate. In this paper, field emission scanning electron microscope and high-resolution transmission electron microscope observations on the red clay-loess-paleosol of the Renjiapo profile at Lingtai, Gansu Province indicate that palygorskite occurs widely in red clay sequences formed before 3.6 Ma, but no occurrence has been found in eolian sediments since 3.2 Ma. Micromorphological features and microstructure of palygorskite show that it is an autogenic mineral formed during pedogenesis, and transformed from iilite-montmorilionite under the pore water action. In the Lingtai profile, the disappearance horizon of palygorskite is consistent with those of increasing magnetic susceptibility, dust flux and depositional rate. The distribution of palygorskite in the profile indicates that the interval of around 3.6 Ma was an important transformation period of the East Asian paleomonsoon, when changes took place in the East Asia paleoclimate pattern, i.e. a high-frequency strong fluctuation alternative evolution of the environment. Therefore, palygorskite is a key indicator mineral of the East Asian paleomonsoon evolution of that time.  相似文献   

建立影像地图集生产系统,提高实践性教学质量     

唐三林  王光霞  谢耕 《测绘工程》2008,17(2):77-80

结合《苏州市影像地图集》的设计和研制,着重讨论基于新技术进行影像地图集生产的软硬件环境,以及通过对新技术的生产流程、过程控制方法等关键环节的技术研究和实践,建立了影像地图集生产实践教学系统。该系统为教师提供了先进的科学研究、技术开发和技术应用环境和条件,为开展实践性教学和进行地图集设计、生产提供理论和技术指导。  相似文献