辫状河致密砂岩储层构型单元定量表征方法

针对现有辫状河储层构型单元定量表征方法关键参数获取困难且可靠性存疑的问题,以储层构型理论为指导,基于现代辫状河沉积、钻井岩心、录井和测井等资料,提出了基于单一辫状河道宽度的构型单元定量表征方法。首先,根据单井构型单元解释结果,确定同期辫状河道平面分布;其次,根据连井对比剖面,确定连井剖面内单一辫状河道间的界线位置;再次,根据现代辫状河单一辫状河道宽度与构型单元关系定量模型,限定辫状水道宽度、复合心滩长度及宽度等4级构型单元规模;最后,在单一辫状河道内确定4级构型单元平面分布,进而在密集井网区对复合心滩进行解剖,确定单个心滩位置和几何形态。采用该方法对苏××提高采收率试验区盒₈^下_1-3单层辫状河致密砂岩气藏进行了分析,结果表明：该单层砂岩气藏发育5条单一辫状河道,其宽度为1 050~1 890 m;辫状水道宽度为234~435 m;复合心滩长度和宽度分别为1 931~3 569 m、685~1 242 m;单个心滩长度和宽度分别为660~1 880 m、310~1 030 m。     

基础地理信息跨尺度联动更新规则体系研究

系统介绍了基础地理信息跨尺度联动更新关键技术相关的规则体系,通过图层映射、几何对应、图面综合、要素取舍、关系协调等多套规则的有机结合,实现了变化更新信息的准确提取;同时开展了基于增量的要素编辑与自动化标注的约束性规则研究,并以1：1万DLG数据联动更新1：5万DLG数据为例,进行了跨尺度基础地理信息联动更新试验。     

从储层构型到“地震构型相”——一种河流相高精度概念模型的表征方法

碎屑岩油气储层构型是指不同级次储层构成单元的形态、规模、方向及其叠置关系。由Miall(1985)运用于河流相储层表征。碎屑岩油气储层构型是储层非均质性的直观表现,直接影响到油气藏开发效果,如何进行精细构型表征是关系到能否正确量化开发指标、或者能否正确描述剩余油分布进而有效减少低效井比例的关键因素。针对渤海明化镇组河流相沉积储层厚度低于地震分辨率的先天不足,对各种构型在地震数据约束下可分辨尺度上进行分类,形成3种构型7类样式的分类体系:垂叠型、侧叠型和孤立型3种砂体构型,垂叠型、密接触侧叠型、疏散接触侧叠型、离散接触侧叠型、下切侵蚀河道孤立型、决口扇孤立型、孤立河道7类样式。研究了每类构型的地震响应特征,阐述了地震属性描述图版,概括了"地震构型相"将构型类型与地震响应有机结合,构建了基于地震构型相的高精度概念模型表征方法。鉴于目前地质建模和数模技术前提下无法对各类储层构型很好地网格化,建立"等效意义"的概念模型开启了一种很好的技术途径。     

Ground penetrating radar for facies architecture and high-resolution stratigraphy: Examples from the Mesoproterozoic in the Chapada Diamantina Basin,Brazil

Ground Penetrating Radar (GPR) surveys were conducted on Mesoproterozoic eolian, fluvial, deltaic, estuarine, and shallow marine successions in the Chapada Diamantina Basin. The subsurface continuation of facies and facies architecture exposed on road cuts was imaged using the GPR signal of a 400-MHz antenna penetrating 8 m in depth, even with mudstone intervals. Reflection patterns in the GPR profiles that were compared with photo mosaics of outcrops and supporting data from vertical sections and gamma ray logs, reveal sedimentary, stratigraphic, and structural features, such as sedimentary structures, the external geometry of architectural elements, stratigraphic surfaces, folds and tension gashes. The patterns most likely reflect the response from low-weathered, non-porous muscovite-illite-rich mudstone and quartzarenite sandstone in which authigenic and detrital illite and sericite are prevalent clay minerals.Measured vertical sections and radar stratigraphy indicate high-frequency cyclic successions of estuarine and shoreface intervals are present at the base of the Tombador Formation. The shoreface intervals are composed of heterolithic strata and offshore tidal bars deposits. The heterolithic shoreface strata exhibit tabular geometry that can be easily identified throughout the outcrop and in the subsurface. Such intervals represent the end of high-frequency transgressive cycles, and hence they are potential candidates for including the maximum flooding surfaces and for defining genetic sequences. Therefore, GPR proved to be an independent method for studying facies architecture and the establishment of a high-resolution stratigraphic framework even in the Precambrian.     

The study of deep water submarine reservoir in Bangle Bay Basin

Although the huge potential of the Bangle Bay Basin has been proven by a series of discoveries, recent drilling and other studies still have not demonstrated the mechanism of hydrocarbon accumulations in Bangle Bay Basin because of the low exploration degree and less geological data available. So, it is difficult to identify and predict the distribution patterns of the main gas reservoir by now. Based on a review of previous work and the latest exploration activities in the study area, the depositional environment and reservoir distribution had been discussed, and thereby assess the location of reservoir–seal couplets for the purposes of stratigraphic traps identification and prospect evaluation within the study area. This paper has also discussed the sequence stratigraphic framework, depositional environment, and facies features by using the biostratigraphic, geochemical analyses and wireline, image logs data. Various broad depositional environments and depositional subsettings have been identified or updated, meanwhile some new environment modeling had been proposed. In this article, reservoir geology study had been conducted after regional depositional feature analysis. Reservoir architecture had been summarized as mouthbars, submarine canyon fill, submarine channels, and levees. Most prospective reservoir intervals identified within the study area are in the Lower Pliocene, Upper Pliocene, and Lower Pleistocene formations.     

空间数据仓库体系结构框架的概念模型

讨论了空间数据仓库的体系结构框架概念模型,主要对空间数据仓库体系结构框架模型中的实体结构、理论技术基础和层次结构等相关问题进行了分析,以期提供构建空间数据仓库应用环境的解决方案。     

WebGIS几种体系结构研究

对于三种常用的GIS体系结构C／S模式、B／S模式和C／S与B／S的混合模式作了详细的比较,对于各自的优缺点作了详细的分析。     

测绘地理信息行业职业技能竞赛信息化评判系统构建

提出了一种针对测绘地理信息行业职业技能竞赛的信息化评判系统构建方法,该方法以网络通信技术、数据库技术、信息技术和地理信息数据质量理论为基础,以"一个管理平台+N个评判子系统"为系统总体模式,以分层架构为系统基本技术架构,以算子集群为评判功能实现模式,扩展性强,功能灵活,可有效消除人为因素对评判结果的干扰,并大幅提高裁判工作效率,系统已在全国推广应用。     

面向虚拟现实的古建筑优化建模技术初探

分析了古建筑共性特点,探讨了几何优化与纹理优化技术,实现了以乐山大佛为核心的大型景区古建筑群的优化建模。     

基于语义P2P的地理共享网络中地理服务发现机制

为了消除集中式SOA系统的"单点故障"问题,本文把语义P2P技术和SOA相结合,不再采用SOA的UDD I进行服务的集中式发布,而是在P2P网络上进行分布式服务发布。通过在语义P2P网络上构建SOA系统,利用P2P的优势进行服务的快速发现和获取,同时也利用地理语义推理解决了地理服务发现中的语义冲突问题。为了实现SOA和语义P2P结合的透明性和平滑性,本文把SOA的服务总线扩展为地理服务总线,地理服务总线基于语义P2P进行服务发现,新的服务发现机制在GSB内部实现,对挂接在GSB上的服务透明,服务间还是按同样的方式交互,因而基于SOA的遗留系统能够平滑升级。通过把地理语义P2P引入SOA,既能发挥SOA在解决大规模分布式异构地理共享系统间的互操作性和服务的透明使用方面的优势,又能利用语义P2P实现地理服务的自动快速发现,从而为大规模的地理共享网络系统建设提供了一条新的思路。