数字专题图形快速编辑方法探讨

以扫描形成的数字矢量底图为基础，对建立沙漠化专题图形库系统中耗资最大的图形编辑问题进行了系列研究，并在以图形工作站和微机组成的分布式网络系统中，形成了可用于建立沙漠化专题图形库的图形快速编辑系统     

关于遥感技术在地质工作中应用的一些问题思考

本文论述了遥感技术在地质工作中应用的8个方面问题,即遥感技术在地质工作中的作用的认识问题、遥感解译和信息提取问题、环形构造问题、影像变异问题、地质体可解译程度问题、影像异常问题、透视信息问题以及遥感地质影像模型问题。文中对上述问题的目前研究现状及今后研究方向进行了初步分析,并提出了个人的初步见解。     

用T106数值产品制作甘肃省极端温度逐日滚动预报

运用T10 6模式的数值产品历史资料 ,用逐步回归方法 ,制作了甘肃省 19个站春、夏、秋、冬四季的最高、最低温度的 2 4h、4 8h、72h、96h和 12 0h时效的预报方程 ,并于 2 0 0 0年 4月投入业务试运行 ,预报结果较好。     

遗传BP算法在洛带气田测井物性解释中的应用

应用遗传算法(GA)对BP网络进行了改进，并在此基础上，利用多种测井数据及岩心描述资料作为网络模型的学习样本，以测井解释渗透率等参数的神经网络模型为例，通过网络的学习、训练，建立了神经网络模型．应用此模型计算物性参数值，解释结果及精度均令人满意．     

REVIEW ARTICLE MULTIVARIATE EXPLORATORY DATA ANALYSIS AND GRAPHICS:A TUTORIAL

Exploratory data analysis(EDA)is a toolbox of data manipulation methods for looking at data to seewhat they seem to say,i.e.one tries to let the data speak for themselves.In this way there is hope thatthe data will lead to indications about'models'of relationships not expected a priori.In this respect EDAis a pre-step to confirmatory data analysis which delivers measures of how adequate a model is.In thistutorial the focus is on multivariate exploratory data analysis for quantitative data using linear methodsfor dimension reduction and prediction.Purely graphical multivariate tools such as 3D rotation andscatterplot matrices are discussed after having introduced the univariate and bivariate tools on which theyare based.The main tasks of multivariate exploratory data analysis are identified as'search for structure'by dimension reduction and'model selection'by comparing predictive power.Resampling is used tosupport validity,and variables selection to improve interpretability.     

活动断裂的遥感影像研究

本文以遥感信息作为研究活动断裂的依据，探讨了利用不同种类、不同比例尺遥感图像分析活动断裂的方法、程序和效果。     

大地电磁技术测定的准噶尔盆地乌伦古坳陷至北隆起带石炭系及油气前景分析

【研究目的】 本文以准噶尔盆地乌伦古坳陷至乌伦古北隆起带为研究区,研究石炭纪地层沉积、分布特征,为该区地质结构研究和油气勘查工作提供了依据和参考。【研究方法】 采集大地电磁测深数据,结合以往重磁电震资料,采用二维共轭梯度反演、最优化电性分层等技术获取石炭纪地层、断裂构造展布特征,为火成岩覆盖区研究石炭纪地层提供了有效的方法。【研究结果】 利用大地电磁测深技术结合重磁电震资料开展综合处理分析,获得研究区石炭系厚度图、石炭系埋深图,初步确定了上下石炭统的分界面,查明了石炭纪地层的分布特征,索索泉凹陷、福海坳陷和扎河坝坳陷为3个石炭纪地层沉降中心,具有较好的油气勘查前景。【结论】 在火成岩覆盖区,采用大地电磁测深、重磁电震综合处理解释技术为石炭纪地层研究提供了有效的技术支撑。     

The Black Sea basins structure and history: New model based on new deep penetration regional seismic data. Part 1: Basins structure and fill

This work is based upon results of interpretation of about 8872 km-long regional seismic lines acquired in 2011 within the international project Geology Without Limits in the Black Sea. The seismic lines cover nearly the entire Black Sea Basins, including Russia, Turkey, Ukraine, Romania and Bulgaria sectors. A new map of acoustic basement relief and a new tectonic structure scheme are constructed for the Black Sea Basins. The basement of the Black Sea includes areas with oceanic crust and areas with highly rifted continental crust. A chain of buried seamounts, which were interpreted as submarine volcanoes of Late Cretaceous (Santonian to Campanian) age, has been identified to the north of the Turkish coast. On the Shatsky Ridge, probable volcanoes of Albian age have also been recognized. Synorogenic turbidite sequences of Paleocene, Eocene and Oligocene ages have been mapped. In the Cenozoic, numerous compressional and transpressional structures were formed in different parts of the Black Sea Basin. During the Pleistocene–Quaternary, turbidites, mass-transport deposits and leveed channels were formed in the distal part of the Danube Delta.     

遥感技术在松潘县第二次土地调查中的应用

本文以1：10000标准分幅数字正射影像图（DOM）为载体,结合松潘县的地形地貌特征、植被分布规律和经济状况等数据,1：50000更新调查成果图,1：100000地形图,包括省、市、县等各级境界与乡、村等土地权属界线,以及土地利用现状数字线画图（LUDLG）为参考,采用内业解译和外业核实、补充调查相结合的方法,探讨与分析了影像解译过程中出现问题及所采取的思路与解决办法。     

A rock physics model to map gross lithology using compaction

Differential compaction has long been used by seismic interpreters to infer subsurface geology using knowledge of the relative compaction of different types of sediments. We outline a method to infer the gross fraction of shale in an interval between two seismic horizons using sandstone and shale compaction laws. A key component of the method involves reconstruction of a smooth depositional horizon by interpolating decompacted thicknesses from well control. We derive analytic formulae for decompaction calculations using known porosity–stress relations and do not employ discrete layer iterative methods; these formulae were found to depend not only upon the gross fraction of shale but also on the clay content of the shales and the thickness of the interval. The relative merits of several interpolation options were explored, and found to depend upon the structural setting. The method was successfully applied to an oil sands project in Alberta, Canada.