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51.
含油气盆地成藏期分析理论和新方法   总被引:80,自引:2,他引:80  
传统的成藏期分析主要从生、储、盖、运、聚、保各项参数有效配置,根据构造演化史、圈闭形成史与烃源岩生排烃史作出推断,常用的 3个方法是根据油源岩的主生油期、圈闭形成期、油藏饱和压力分析油气藏形成期。近10年来成藏期分析是在构造发展史、埋藏史、热演化史、沉积成岩史 4个方面地质历史分析基础上,更多地依靠成藏化石记录的地球化学和岩石学分析结果,获得成藏期定量数据。评述了成藏期定量分析的理论与方法:包括储层成岩作用与烃类流体充注序次、自生矿物同位素地质年代学、流体包裹体、储层磁性矿物古地磁学、生烃期精确分析等,并讨论了它们在叠合盆地成藏年代学分析中实际应用及存在问题。  相似文献   
52.
刘旭 《北京测绘》2020,(5):610-613
针对地下管网隐患数据管理的应用需求,本文基于三维平台设计实现了地下管网健康档案管理平台,在三维场景加载地上精细模型和地下管网数据,以三维可视化的手段对管网各类隐患问题进行信息管理,结合二维GIS操作,实现了净距分析、覆土分析、占压分析等管线隐患分析功能,通过本平台建立的地下管网健康档案数据库,方便用户对各类管网隐患数据进行信息管理和统计,为管道病害修复、管网改造提升提供数据支撑,保证地下管网的安全运行。  相似文献   
53.
ABSTRACT

National and regional water quality monitoring networks have been operated in South Africa since the early 1970s. These originally had text-based inventories that were convenient for specialists who were familiar with the national networks and knew the locations of their sites of interest. However, within two decades the networks had expanded in geographical extent and variables monitored to such an extent that users needed spatial context in order to locate sites that fitted their information requirements. Mapping applications running on the Internet, such as Google Earth and Leaflet, form the foundation of a system for providing online inventories and summaries of the data available on the water quality database. The interfaces were constructed using available software, mainly ArcInfo and R. A recent concern is a decrease in the collection of water quality data, which is reducing the value of data summaries for water resource management.  相似文献   
54.
ABSTRACT

Large-sample hydrology (LSH) relies on data from large sets (tens to thousands) of catchments to go beyond individual case studies and derive robust conclusions on hydrological processes and models. Numerous LSH datasets have recently been released, covering a wide range of regions and relying on increasingly diverse data sources to characterize catchment behaviour. These datasets offer novel opportunities, yet they are also limited by their lack of comparability, uncertainty estimates and characterization of human impacts. This article (i) underscores the key role of LSH datasets in hydrological studies, (ii) provides a review of currently available LSH datasets, (iii) highlights current limitations of LSH datasets and (iv) proposes guidelines and coordinated actions to overcome these limitations. These guidelines and actions aim to standardize and automatize the creation of LSH datasets worldwide, and to enhance the reproducibility and comparability of hydrological studies.  相似文献   
55.
A series of Hokkaido events, recorded by the FBV Broadband Seismograph System at the KHC Seismic Station, is used to study the structure of the earthquake magnitude scale on the basis of maximum velocity amplitudesA vmax of teleseismicPwaves in different period bands. Amplitude-periodband (APB) diagrams are constructed for each event. According to the shape of the APB diagrams the events investigated can be divided into three types: (a) events with largestA vmax values in the intermediate period range (periods ofA vmax from 2.2 to 23 sec), (b) events with largestA vmax values in the short-period range (periods ofA vmax from 1 to 2 sec), (c) events exhibiting anomalous APB diagrams. Type (a) events seem to represent the process of wave generation that prevails for shallow earthquakes. Type (b) events approach to explosive-like generation of seismic waves. The nature of the exceptionally occurring type (c) events must be clarified in further investigations. The influence of the type of earthquake on the magnitude values estimated on the basis of standard class A and B (short-period and intermediate-band) seismograms is demonstrated. It appears that for estimating correct values of earthquake magnitudes complementary information on the process of seismic wave generation in the focus is necessary. At teleseismic distances this information can be obtained from either APB diagrams or amplitude spectra ofP waves recorded, e.g., by broadband velocity sensing instruments.  相似文献   
56.
热对流成岩作用的基本特征与研究意义   总被引:18,自引:1,他引:18  
介绍了热对流产生的条件与地质背景,指出火成侵入体、盐丘和活跃断层周围等温线陡倾斜场所易发生热对流成岩作用。综述了岩浆成因热对流的岩石学记录,包括热变质作用、突然升温—逐渐降温的自生矿物组合和相对高温的自生矿物类型,分析了自生伊利石的K/Ar年龄在热对流成岩作用研究中的作用。阐述了热对流成岩作用对盆地动力学、砂岩储层和油气运移研究的意义。  相似文献   
57.
EXTREMERESERVOIRSEDIMENTATIONINAUSTRALIA:AREVIEWHubertCHANSON1ABSTRACTInthepaper,theauthorreviewstheproblemofreservoirsiltati...  相似文献   
58.
In 1876 Blytt proposed a post-glacial climatic classification, maintaining that the then temperature fluctuated 1- 2℃ higher or lower than that today. Lamb (1969) held that in Europe " the axis of the subtropical high pressure belt was generally displaced north by about 10° latitudes" during the Hypsithermal and that the temperature was three to six times higher than that in the postglacial period.In China, there appear relict beachrocks (living fossils) in tropical tidal zones from the Bohai Bay (40° N) to coastal areas in South China. Many relict tropical marine fossils were discovered, such as Ostrea gigas in Tianjin (which is larger than that found today in Hainan), Placuna placenta in Zhejiang and Spondylus sp. in Fujian. In Hebei, Henan and Zhejiang provinces and Guilin of Guangxi, such tropical fossil animals as Elephas maximus and Rhinoceros sp, were discovered, and in Hebei and Jiangsu provinces such fresh water fossils as Unio douglasiae were found. Their living species are still seen in So  相似文献   
59.
从地层记录的特性论岩石地层学的困惑   总被引:24,自引:7,他引:17  
梅冥相 《地层学杂志》1996,20(3):207-212
地层记录有四个特性:不完整性、非渐变性、旋回性及复杂性。这四个特性在岩石地层中将形成两种穿时性——相界面穿时及间断面穿时,最终造成常规标志层的缺乏和复杂有序的相变。为此,根据"岩性、岩相的统一"来划分和对比岩石地层单位时,常常具有人为性及不确定性。在相序基础上识别出的旋回层序,具有空间上相序的有序性及时间上环境变化的同步性两大特征,在把它用于岩石地层学研究时,具有以下优点:1)不同级别旋回层序及其有序叠加形式的研究是从岩石地层记录的复杂性中寻找规律的最好方法;2)旋回层序,特别是长周期旋回层序的界面,同样可以作为岩石地层单位的界面;3)地层记录的旋回性的研究,可以丰富岩石地层单位的的内容,为其划分对比提供更多的天然标志。  相似文献   
60.
本项研究是PMIP(PalaeoclimateModelingIntercomparisonProject)国际合作项目中有关模型模拟与观测资料对比的一部分。模型试验对象是6000yr.BP的全球湿润状况。模拟试验以检测太阳辐射变化对全球大尺度气候系统的影响为主要目的。观测资料是利用地质证据恢复的古湖泊水位变化,实际上是某一地区的有效降水(降水减蒸发)的变化。通过两者的比较发现,所有模拟试验均能重现6000yr.BP在亚洲南部与非洲北部的湿润环境,从而证实了因太阳辐射变化导致的亚洲与非洲季风的增强。但模拟的季风增强无论是强度还是范围均小于地质记录。原因很可能是模拟试验中下垫面特征用“现代”的来处理。模拟试验对北半球夏季辐射增加造成的西风带北移及由此引起的中纬度地区的气候变化不够成功。绝大多数模拟对受洋流与海温影响较大的地区是失败的。主要原因可能是所有PMIP中的模拟试验都未考虑海洋的作用。  相似文献   
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