不同煤阶煤层气运移通道的差异性研究     

王庆伟  王勤旺 《中国煤炭地质》2012,(4):24-26,30

不同煤阶运移通道的差异性研究可对煤层气开发工艺的选择和参数的确定具有重要的理论意义和指导生产的实际意义。利用达西渗流理论,判定了煤层气流态和渗透率之间的关系,进而借助实验室方法测定了不同煤阶煤储层的渗透率,最终利用煤层气流态建立了煤储层渗透率与运移通道的关系,总结出了不同煤阶煤层气运移通道的差异性：①低煤阶：煤储层运移通道是基质孔隙起主导作用;②中煤阶：煤储层运移通道是割理、裂隙并重;③高煤阶：煤储层运移通道是裂隙起主导作用。  相似文献   

苏里格低渗砂岩大气田天然气充注运移及成藏特征     

李贤庆  李剑  王康东  孔龙玺  冯松宝  黄孝波  王萌 《地质科技情报》2012,31(3):55-62

苏里格气田位于鄂尔多斯盆地伊陕斜坡西北部,属于典型的低渗砂岩大气田.苏里格气田上古生界天然气组分和碳同位素组成特征变化较小,反映其来源和成藏过程的一致性.基于对成藏地质背景、储层物性、天然气地球化学特征、烃源岩成熟度、甲烷碳同位素动力学的综合分析,认为苏里格气田天然气主要为近源充注、近距离运移和聚集,为石炭系一二叠系煤系烃源岩生成的累积聚气.天然气运移输导体系主要包括砂体一孔隙、微裂缝及小断层等,由孔隙和裂缝构成的网状输导体系在成藏过程中起了重要作用,表现为动力圈闭成藏.苏里格气田形成过程经历了早侏罗世末期、晚侏罗世至早白垩世末期、早白垩世末期至今3个演化阶段,存在下生上储和自生自储两种成藏方式.  相似文献   

华北下二叠统太原组Zoophycos潜穴中碳酸盐岩微形体的特征及其意义     

宋慧波  郭瑞睿  王保玉  胡斌 《沉积学报》2014,32(5):797-808

华北地区下二叠统太原组碳酸盐岩中的Zoophycos遗迹化石十分丰富,根据其潜穴充填物颜色的不同,可将太原组Zoophycos分为四种类型,即具黑色、灰色、灰白色、红色充填物的Zoophycos。本文选取河南焦作和山西附城太原组剖面中具有代表性的Zoophycos样品,利用扫描电子显微镜和能谱仪对其潜穴中的充填物进行了超微特征观察及元素组成测定,发现了大量成因与微生物相关的碳酸盐岩微形体（单体矿物和集合体）,识别出球状（表面光滑的球状体、表面具有不定形细粒结构的球状体、表面呈刺状细粒结构的球状体和球状集合体）、杆状（刺杆状分枝形网状体、刺杆状单体、螺旋杆状单体、双列杆状体、光滑直线形杆状单体、末端膨大的光滑杆状体）、簇状、网状、瓶状和似脑球状等6种形态类型,其中多数显示出不同的微生物结构。这一发现表明,Zoophycos遗迹化石并非简单的觅食迹或食物储藏所,其造迹生物与微生物很可能存在互利共生关系。此次研究有助于探索地质微生物作用对地球化学过程的影响,并为精细分析该研究区太原组碳酸盐岩的形成过程及其沉积演化提供了微观资料。  相似文献   

Carbon and sulfur isotopic fluctuations associated with the end-Guadalupian mass extinction in South China     

《Gondwana Research》2014,25(3-4):1276-1282

Concentrations of total organic matter (TOC), carbon isotopic compositions of carbonate and organic matter (δ¹³C_carb, δ¹³C_org), and sulfur isotopic compositions of carbonate associated sulfate (δ³⁴S_sulfate) across the Guadalupian–Lopingian (G–L) boundary were analyzed from identical samples of Tieqiao section, Laibin, Guangxi province, South China. The δ¹³C_carb values show a positive excursion from − 0.45‰ to the peak of 3.80‰ in the Laibin limestone member of the Maokou Formation, followed by a drastic drop to − 2.60‰ in the lowest Heshan formation, then returned to about 1.58‰. Similar to the trends of the δ¹³C_carb values, Δ¹³C_carb–org values also show a positive excursion followed by a sharp negative shift. The onset of a major negative carbon isotope excursion postdates the end Guadalupian extinction that indicates subsequent severe disturbance of the ocean–atmosphere carbon cycle. The first biostratigraphic δ³⁴S_sulfate values during the G–L transition exhibit a remarkable fluctuation: a dramatic negative shift followed by a rapid positive shift, ranging from 36.88‰ to − 37.41‰. These sulfate isotopic records suggest that the ocean during the G–L transition was strongly stratified, forming an unstable chemocline separating oxic shallow water from anoxic/euxinic deep water. Chemocline excursions, together with subsequent rapid transgression and oceanic anoxia, were likely responsible for the massive diversity decline of the G–L biotic crisis.  相似文献   

基于ObjectARX的船舶建造可视化测控系统研制     

魏叶青  岳建平  方露 《现代测绘》2011,34(1)

以CAD为平台,C#为开发环境,介绍了基于ObjectARX的船舶建造可视化测控系统的开发流程。详细阐述了系统整体架构,分析了该系统开发的关键技术。工程实际应用结果表明,该系统操作简单、实用,能够满足船舶建造测控高精度、可视化等的要求。  相似文献   

西南天山前缘乌拉根背斜南翼逆断层的发现及其地质意义   总被引：2，自引：1，他引：1       下载免费PDF全文

李涛  陈杰  肖伟鹏  Burbank D W  Thompson J  杨晓东 《地震地质》2011,33(2):277-288

塔里木盆地新疆喀什以西部分是西南天山和帕米尔两大对冲构造系统的会聚带,关于两者变形前缘和分界的确切位置存在不同认识.在乌恰县以南的玛依卡克盆地南缘,清晰可见属于帕米尔构造带、向N或NNE逆冲的帕米尔前缘逆冲推覆体(PFT).最近野外调查在盆地北部发现了西南天山前缘的最新变形带:向南逆冲的乌拉根背斜南翼断层.断层总体近E...  相似文献   

Changes of land cover in the Yarlung Tsangpo River basin from 1985 to 2005   总被引：1，自引：0，他引：1  

Fapeng Li  Zongxue Xu  Youcan Feng  Mei Liu  Wenfeng Liu 《Environmental Earth Sciences》2013,68(1):181-188

Land cover is closely related to environmental changes and socioeconomic development. Land-cover change in the Tibetan Plateau (TP) is different from that in the lowlands; however, a detailed land-cover change in areas such as the Yarlung Tsangpo River (YTR) basin in the TP has not been reported. To fill this gap, the current study explores the land-cover change between 1985 and 2005 in the YTR basin. The results show that only 1 % of the land cover in the YTR basin changed during this time period. The most significant land-cover changes included increases in forest and built-up areas as well as decreases in grassland, water and wetland areas. By percentage, the most rapid land-cover change occurred for built-up areas with an annual variation of 2.07 %. There was an obvious vertical distribution pattern for land-cover types in the YTR basin; from low to high, the average altitudes were forest, farmland, built-up, grassland, water and wetland, and bare land. The average altitude and slope for most land-cover types did not vary over the past 20 years. However, the average altitude and slope of built-up significantly decreased, especially in the zone between 3,500 and 4,000 m. The water and wetland area in altitudes above 4,500 m increased; however, they decreased in the zone between 3,500 and 4,000 m. Natural factors cause most land-cover changes, whereas the increasing intensity of human activities cause some changes to built-up and farmland. Additional attention should be paid to the study of the mechanism of land-cover change in the TP.  相似文献   

Revision of P-wave velocity and thickness of hydrate layer in Shenhu Area,South China Sea     

Jianming Gong  Xunhua Zhang  Changchun Zou  Qiang Chen  Lichen Wang  Chunfang Yuan  Gaowei Hu  Yubo Jiang 《中国海洋大学学报(英文版)》2014,13(5):742-746

To revise P-wave velocity and thickness of the hydrate layer in the Shenhu area of the South China Sea, acoustic and resistivity logging curves are reanalyzed. The waterlogging phenomenon is found in the shallow sediments of five drilling wells, which causes P-wave velocity to approximate the propagation velocity of sea water(about 1500 m s-1). This also affects the identification of the hydrate layer and results in the underestimate of its thickness. In addition, because there could be about a 5 m thick velocity ramp above or below the hydrate layer as interpreted by acoustic and resistivity logging curves, the recalibrated thickness of this layer is less than the original estimated thickness. The recalibrated P-wave velocity of the hydrate layer is also higher than the original estimated velocity. For the drilling well with a relatively thin hydrate layer, the velocity ramp plays a more important role in identifying and determining the thickness of the layer.  相似文献   

基于行为聚类算法的土地利用聚类适宜性分析研究     

孙云华  郭涛  崔希民  崔伟宏 《地球信息科学学报》2016,18(3):396-405

为了在较少地类的基础上,深入研究土地利用变化过程,可把较多的地类合并成较少的具有重要变化特征的地类.本文运用基于行为聚类的方法,将净增加和净增加的地类合并或净减少和净减少的地类合并,但不能将净增加和净减少的地类合并.主要分为3个阶段实现:第1个阶段是完全不变阶段,聚类结果是形成综合的完全不变地类;第2个阶段是完全减少和完全增加阶段,该阶段将完全减少地类和完全增加地类分别进行合并;第3个阶段是转变阶段,该阶段计算了每一对有相同净变化方向地类的相互转变信息.基于行为聚类的算法在每一步的计算过程中都会保留净变化面积为常数,转变变化面积保留最大化.本文对3个聚类原则进行了数学证明,定义了6种聚类行为,以云南省土地利用分类体系为例,从面积变化和强度变化2个角度阐述了行为聚类方法的可行性和优势性.最后,与刘纪远等建立的土地利用遥感监测分类系统进行比较,结果表明:行为聚类算法聚类到9种类型时,类型总变化面积达到5.10%,比原始类型的总变化面积下降了0.06%;而基于遥感监测分类系统的6个一级分类将总变化减少至4.7%,与聚类算法比较,总变化面积减少了0.4%.实践证明,行为聚类的算法可更好地保留土地利用动态变化信息,证明了该聚类方法的有效性.  相似文献   

基于符号集合近似的城市轨道交通站点分类研究     

张丽英  孟斌  尹芹 《地球信息科学学报》2016,18(12):1597-1607

轨道站点是城市轨道交通基本线网系统中的关键节点,科学的轨道站点分类,对了解城市功能分区及评价轨道交通基础设施建设情况具有重要意义。轨道交通站点时间序列客观记录了所观测的站点在各个时刻点的重要信息,研究其时间序列聚类,是认识和理解轨道交通站点时间序列形成本质的重要手段,也是挖掘轨道交通站点时间序列中隐含的有较高价值规律知识的重要方法。本文以北京IC卡轨道站点刷卡数据为研究对象,提出了描述轨道站点的4个数据集,即工作日进站数据集(WB)、工作日出站数据集(WA)、休息日进站数据集(RB)和休息日出站数据集(RA);并首次引入时间序列分析方法（符号集合近似(SAX)方法）对4个数据集进行聚类分析,实现了高维数据的有效降维和轨道站点之间的相似性度量。采用层次聚类方法并根据聚类有效性DB指数确定将195个站点分为8类更为合理。通过分析每类站点的日客流特征和空间位置分布情况,为轨道交通站点规划设计和管理服务提供一定的客观参考依据。  相似文献