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71.
综合利用Photoshop、Geoway、MapInfo、ArcView等软件提供的处理技术,通过对扫描得到的地形、土地利用和水土流失等要素图进行图像剪切、拼接、配准、采样、跟踪、调整以及属性表的维护等一系列处理步骤,建立了大比例尺小流域地理空间框架数据集,提供了小流域空间框架数据采集与应用的技术流程与方法,提出应用各种软件进行大比例尺空间框架数据处理过程中应当注意的各种细节问题.最后,以闽南丘陵地区草子坝小流域为例,利用ArcView的3D Analyst、Spatial Analyst、Geoprocessing等扩展模块以及MapInfo SQL查询功能,对流域空间框架数据进行处理,得到了用于比较精细空间尺度上表达流域三维地形模型、坡度、坡向、河流垂直剖面、晕渲,不同高程上的土地利用类型等专题应用结果. 相似文献
72.
地震应急指挥辅助决策系统 总被引:2,自引:0,他引:2
本系统将地震应急辅助自动化和人工应急数据处理有机结合于一体 ,能在地震震中定位后几十秒内自动生成震中位置图、裂度线分布图 ,完成震害快速分级评估 ,及应急具体详细方案选择 ,并能随应急工作进展快速调整应急方案、重新评估地震灾害。 相似文献
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阐述了海南省防震减灾中心大楼的地震应急指挥技术系统移植重建构成和主要功能,实现了系统集成化管理功能,在实际应用和演练中收到较好效果. 相似文献
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简要介绍了基于CAD平台开发悬挂点检查与自动处理的程序开发技术、技术路线、实现方法、主要源代码。主要用于地籍测量数据入库前悬挂点检查,并用实例进行了验证,取得了满意的效果,达到了设计的目的,为作业单位提高了效率。 相似文献
78.
WANG Min TIAN Shansi CHEN Guohui XUE Haitao HUANG Aihua WANG Wenguang 《《地质学报》英文版》2014,88(6):1792-1797
Abstract: In China, hot researches on shale oil were raised by the important breakthrough of shale oil in America. Obviously, the first important issue is the actual shale oil resource potential of China, and the selection of the key appraisement parameter is vital to the shale oil resource amount. Among the appraisement parameters, the oil content parameter (S1) is the key one, but the evaluation result is generally lower because of light hydrocarbon losing and heavy hydrocarbon handling. And the more important thing is that the light hydrocarbon with small molecular weight is more recoverable, and therefore its amount is important to the total shale oil yields. Based on pyrolysis experiments and the kinetic model of hydrocarbon generation, correction factors and a model of light hydrocarbon losing and heavy hydrocarbon handling were established. The results show that the correction factor of heavy hydrocarbon handling is 3.2, and that of light hydrocarbon losing is controlled by kerogen type, maturity and hydrocarbon generation environment (closed or open). 相似文献
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《International Geology Review》2012,54(15):1922-1940
Our aim is to determine the mean compositions of modern island and continental arcs, along with dispersion estimates, and use them to evaluate their similarities and differences in such subduction settings. First, following the conventional approach, the statistical parameters of mean, median, and standard deviation were simply calculated from the available combined data from all island or continental arcs. However, it is mandatory to ascertain from significance tests that all island or continental arcs used for these estimates are statistically similar in their compositions before combining the data from different arcs and calculating the mean values and their uncertainties for the chemical parameters of interest. A new computer program, Univariate Data Analysis System (UDASYS), was developed for this purpose because the available programs are not efficient for applying the significance test of analysis of variance (ANOVA) to large numbers of sample groups, as in the present work. Compositional data for 16 island and 12 continental arcs around the world were compiled and processed in UDASYS. The best compositional estimates for all three types of magmas (basic, intermediate, and acid) from island and continental arcs were statistically evaluated to document, for the first time, significant differences for 64–94% of the geochemical parameters under study. These differences in large-ion lithophile elements, light rare earth elements, high-field strength elements, and numerous log-ratios are likely caused by different types of underlying crust beneath island and continental arcs. More specifically, the examination of two nearby arcs, Izu-Bonin (island) arc and Japan (continental) arc, confirmed that about 65–77% of the parameters showed significant differences, which may be related to the different types of crusts beneath these spatially close areas. The differences between the log-ratios of island and continental arc basic magmas further indicate that new multi-dimensional discrimination diagrams can certainly be proposed in future to discriminate such basic magmas from these two very similar tectonic settings, which at present is possible only from diagrams for intermediate and acid magmas. 相似文献