西湖凹陷H构造群及周边花港组沉积环境及砂体刻画     

何苗  侯国伟  秦兰芝  陆嫣  谢晶晶 《现代地质》2018,32(1):162

西湖凹陷H构造群及周边为中央反转带中南部区域大型反转挤压背景下形成的区块,紧邻富凹,具有油气潜力。为了更好地寻找有利勘探区带以及富砂层位,结合地震反射特征、成像测井资料、岩石以及古生物资料对H构造群及周边花港组的沉积背景进行了研究,认为花港组发育于构造稳定的中等水动力环境下,受多向水流影响,孢粉及其他生物组合表明花港组整体处于淡水环境。通过测井、取心资料分析认为花港组为网状河沉积,其中网状水道、交错坝以及纵向砂坝砂体十分发育。此外,结合连井和地震剖面对河道砂体的垂向叠置及展布规律的研究表明,砂体垂向叠置关系以单边对接式、多边对接式及不完全切叠式为主,平面以带状、交织带状和网状形态为主,深部河道砂体具一定规模。  相似文献   

基于浏览器的气象再分析平台通用架构及组件设计     

杜晓宇 《成都信息工程学院学报》2014,29(4):370-375

气象再分析在互联网中的应用还处于起步阶段,缺乏成熟的系统体系及开发标准。为降低开发人员开发气象再分析产品的难度,提升开发效率,同时避免开发人员误解气象用户需求,论文总结国家科技基础条件平台运行服务主系统功能完善项目的开发过程,基于经典的MVC三层模模型,提出面向气象领域的在线再分析平台通用架构,并将架构中数据过滤和数据显示封装为组件。工作以专业气象用户需求设计效果及习惯,以开发人员的开发模式开放配置接口,建立在线平台的开发基础。该成果用于洪水监测预警系统项目的需求分析,开发人员使用通用架构,再通过三步操作:匹配数据源、设计页面布局、配置组件,完成原型开发。以此优化系统架构过程,复用已有组件。  相似文献   

A strategy for raster-based geocomputation under different parallel computing platforms   总被引：1，自引：0，他引：1  

Cheng-Zhi Qin  Li-Jun Zhan  A-Xing Zhu  Cheng-Hu Zhou 《International journal of geographical information science》2014,28(11):2127-2144

The demand for parallel geocomputation based on raster data is constantly increasing with the increase of the volume of raster data for applications and the complexity of geocomputation processing. The difficulty of parallel programming and the poor portability of parallel programs between different parallel computing platforms greatly limit the development and application of parallel raster-based geocomputation algorithms. A strategy that hides the parallel details from the developer of raster-based geocomputation algorithms provides a promising way towards solving this problem. However, existing parallel raster-based libraries cannot solve the problem of the poor portability of parallel programs. This paper presents such a strategy to overcome the poor portability, along with a set of parallel raster-based geocomputation operators (PaRGO) designed and implemented under this strategy. The developed operators are compatible with three popular types of parallel computing platforms: graphics processing unit supported by compute unified device architecture, Beowulf cluster supported by message passing interface (MPI), and symmetrical multiprocessing cluster supported by MPI and open multiprocessing, which make the details of the parallel programming and the parallel hardware architecture transparent to users. By using PaRGO in a style similar to sequential program coding, geocomputation developers can quickly develop parallel raster-based geocomputation algorithms compatible with three popular parallel computing platforms. Practical applications in implementing two algorithms for digital terrain analysis show the effectiveness of PaRGO.  相似文献   

Ecological adaptation of Reaumuria soongorica root system architecture to arid environments     

LiShan Shan  Yi Li  DongMei Geng  QiuLian Dong 《寒旱区科学》2014,6(2):0150-0158

The architectural parameters of Reaumuria soongorica root system in different habitats of Gansu Province, China were analyzed to examine its ecological adaptability to arid environments. Results show that： （1） Topological indices of R. Soongorica root sys- tem are small in all habitats, and root branching pattem tends to be dichotomous. Also, the indices gradually increase in the Min- qin windblown sand region and the Zhangye Gobi region in Hexi Corridor, which indicates that drought tends to produce her- ringbone-like root branching pattems. （2） Fractal dimension values ofR. Soongorica root system are small and not obvious in the Minqin windblown sand region and the Zhangye Gobi region in Hexi Corridor, with values of 1.1778 and 1.1169, respectively. Fractal dimension values are relatively large in Jiuzhoutai semi-arid hilly and gully region of the Loess Plateau, which indicates that the R. Soongorica root system has better fractal characteristics in this region than in the other regions. （3） Total branching ra- tios of the R. Soongorica root system in arid regions of Hexi Corridor are smaller than that in the Jiuzhoutai semi-arid hilly and gully region of the Loess Plateau. This shows that root branching ability in the semi-arid region is stronger, and it decreases to some degree with increased drought. （4） The root connection lengths of R. soongorica root system are long in all habitats, but there are significant length differences between the different habitats. The root connection length at the Minqin windblown sand region is the longest. It is concluded that R. soongoriea adapts to arid environments by decreasing root branching, decreasing root overlap and increasing root connection length, which makes its root branching pattern tend to be herringbone-like to reduce com- petition in root internal environment for nutrients and to enhance root absorption rate of nutrients, and ensure effective nutrition space. Thus the roots can absorb enough water and nutrients in resource-poor settings to ensure normal physiological requirements.  相似文献   

兰坪盆地古近系宝相寺组层序地层分析          下载免费PDF全文

冯志强  郭建秋  阮林森  李诗强  牟业龙  刘文强  密文天 《地质找矿论丛》2012,27(1):103-108

文章运用层序地层学原理,对兰坪盆地中部古近系宝相寺组进行深入研究,划分出1个Ⅰ型层序及3个Ⅱ型层序界面。阐述了兰坪盆地中部古近系宝相寺组层序格架及砂体结构特征,建立层序地层格架演化模式图,反映了湖平面变化对砂体沉积结构的重要影响。低位体系域早期河流侵蚀强烈,多以中粒为主,晚期发育复合状砂体;湖侵体系域砂体多为细粒砂泥岩,呈孤立状形态;高位体系域砂体以席状砂体为主,主要由滨浅湖、半深湖和湖泊三角洲沉积体系构成。  相似文献   

Controls on large‐scale patterns of fluvial sandbody distribution in alluvial to coastal plain strata: Upper Cretaceous Blackhawk Formation,Wasatch Plateau,Central Utah,USA     

GARY J. HAMPSON  M. ROYHAN GANI  HIRANYA SAHOO  ANDREAS RITTERSBACHER  ANDREW RANSON  JOHN A. HOWELL  SIMON J. BUCKLEY  BRYAN BRACKEN 《Sedimentology》2012,59(7):2226-2258

Current models of alluvial to coastal plain stratigraphy are concept‐driven and focus on relative sea‐level as an allogenic control. These models are tested herein using data from a large (ca 100 km long and 300 m thick), continuous outcrop belt (Upper Cretaceous Blackhawk Formation, central Utah, USA). Many channelized fluvial sandbodies in the Blackhawk Formation have a multilateral and multistorey internal character, and they generally increase in size and abundance (from ca 10% to ca 30% of the strata) from base to top of the formation. These regional, low‐resolution trends exhibit much local variation, but are interpreted to reflect progressively decreasing tectonic subsidence in the upper Blackhawk Formation and overlying Castlegate Sandstone. The trend may also incorporate progressively more frequent channel avulsion during deposition of the lower Blackhawk Formation. Laterally extensive coal zones formed on the coastal plain during shallow‐marine transgressions, and define the high‐resolution stratigraphic framework of the lower Blackhawk Formation. Large (up to 25 m thick and 1 to 6 km wide), multistorey, multilateral, fluvial channel‐complex sandbodies that overlie composite erosion surfaces occur at distinct stratigraphic levels, and are interpreted as fluvial incised valley fills. Low amplitude (<30 m) relative sea‐level variations are interpreted as the dominant control on stratigraphic architecture in the lower Blackhawk Formation, which was deposited up to 50 km inland from the coeval shoreline. In contrast, the high‐resolution stratigraphy of the upper Blackhawk Formation is poorly defined, and channelized fluvial sandbodies are poorly organized. Vertical and laterally offset stacking of a small proportion (<10%) of sandbodies produced ‘clusters’ that are not confined by ‘master’ erosion surfaces. Avulsion is interpreted to dominate the stratigraphic architecture of the upper Blackhawk Formation. This data‐driven analysis indicates that alluvial to coastal plain stratigraphic architecture reflects a combination of various allogenic controls and autogenic behaviours. The relative sea‐level control emphasized in sequence stratigraphic models is only rarely dominant.  相似文献   

陆相湖盆层序构型及其岩性预测意义:以珠江口盆地惠州凹陷为例   总被引：1，自引：0，他引：1       下载免费PDF全文

朱红涛  杨香华  舒誉  吴静  李敏 《地学前缘》2012,19(1):32-39

地层岩相组合有规律地分布于层序的不同体系域。为了有效地进行储层发育、烃源岩分布的预测,文中提出层序构型的明确概念、类型、识别标志及其意义。层序构型是指三级层序内不同体系域地层单元时间-空间组成配置关系,其类型可分为L型、T型、TH型、H型(E-H型和L-H型)4种,其中,L型层序主要为富砂层序,储层相对发育;T型层序为富泥层序,烃源岩最为发育;TH型层序为富泥层序,烃源岩相对发育;E-H型层序为富泥层序,烃源岩发育程度次于TH型层序;L-H型层序主要为富砂层序,储层相对发育。珠江口盆地富烃的惠州凹陷文昌组层序构型实例分析表明,惠州凹陷南缘主要为T型层序,烃源岩相对发育,北缘主要为H型层序,储层相对发育。  相似文献   

地下储层构型表征:现状与展望   总被引：3，自引：0，他引：3       下载免费PDF全文

吴胜和  翟瑞  李宇鹏 《地学前缘》2012,19(2):15-23

地下储层构型表征是近十几年发展起来的油气藏开发地质研究方向。与露头构型分析不同的是,地下储层构型表征主要依据地震信息和多井信息,相应地发展了两类方法,其一为地震沉积学(地貌学)方法,即通过三维地震资料地层切片等方式,利用地震成像特征研究沉积单元的分布;其二为多井模式预测方法,即通过将不同级次的定量构型模式与地下井资料(包括动态监测资料)进行拟合,分级约束并预测不同级次的构型单元的井间分布。论述了这两类方法的起源、基本原理、应用范畴及存在问题,并根据油田生产要求与技术发展提出了进一步深入研究的方向,包括三维定量构型模式的深化研究、储层构型地震响应及解释方法研究、多井模拟拟合方法的改进与创新等。  相似文献   

Sedimentary facies and stratigraphic architecture in coarse-grained deltas: Anatomy of the Cenozoic Camaná Formation,southern Peru (16°25′S to 17°15′S)     

《Journal of South American Earth Sciences》2014

In the external forearc of southern Peru (Arequipa region), the sedimentary facies and the stratigraphic architecture of the Cenozoic Camaná Formation are presented in the context of tectono-eustatic controls. The Camaná Formation is defined as ∼500 m thick coarse-grained deltaic complex that accumulated in a fault-bounded elongated depression extending from the Coastal Cordillera in the east to the offshore Mollendo Basin in the west and likely up to the Peruvian Trench. Based on the analysis of facies associations, we propose a refined stratigraphic scheme of the Camaná Basin fill. The Camaná Formation was formerly divided into the Camaná “A” and Camaná “B” units (CamA and CamB, respectively). We reinterpret the stratigraphic position and the timing of the CamA to CamB boundary, and define three sub-units for CamA, i.e. sub-units A1, A2, and A3. Each depositional unit shows individual stacking patterns, which are linked with particular shoreline trajectories through time.Strata of A1 form the basal succession of the Camaná Formation and consist of distributary channels and mouth bars, unconformably overlain by beds of A2. A2 consists of delta front deposits arranged in voluminous clinothems that reflect a progradational downstepping complex. A3 consists of delta front sandstones to prodelta siltstones arranged in retrogradational onlapping geometry. A pebbly intercalation in proximal onlapping A3 deposits is interpreted to reflect pulses of uplift in the hinterland. The overlying CamB unit is characterized by a thick alternation of fluvio-deltaic conglomerates and sand bars. The ages of the individual units of the Camaná Formation are not yet well defined. Based on the available information and stratigraphic correlations we tentatively assign A1 to the Late Oligocene, A2 to the Early Miocene, A3 to the late Early Miocene to early Middle Miocene, and CamB to the Late Miocene to? early Pliocene.The sub-units A1 and A2 represent a regressive systems tract, where the shoreline was forced to migrate seaward. This scenario differs from the Early Miocene eustatic sea-level rise suggesting that significant tectonic uplift along the Coastal Cordillera controlled the high sediment influx during A2 deposition. The sub-unit A3 represents a transgressive systems tract, triggering landward migration of the shoreline. This scenario is well in line with the global sea-level chart suggesting that A3 has been deposited during a phase of eustatic sea-level rise with minor tectonic activity. The fluvial deposits of CamB reflect an increased sediment flux due to uplift of the hinterland. The observed stratigraphic patterns support predominant tectonic control on sedimentation in the Camaná Basin and the established stratigraphic framework provides an essential baseline for future correlations of the Cenozoic sedimentation in the forearc area of the Central Andes.  相似文献   

Architecture and composition of the Upper Burdigalian z-coral build-ups of southern Corsica (Mediterranean)     

《Comptes Rendus Geoscience》2014,346(1-2):45-51

In southern Corsica, three successive Upper Burdigalian coral reef episodes (R1, R2 subdivided into R2A and R2B subunits, and R3) developed within the Cala di Labra Formation. Tabular corals dominated under high water energy and siliciclastic input conditions. The R1 reefs show the highest coral diversity with 16 species described for the first time. A coral impoverishment was recorded in the R2 and R3 reefal episodes. The reefs did not reach a climax growth stage, except the R1 ones. Analogous to North Sardinian reefs, they reflect local vanishing conditions in the Corsican–Sardinian block through Upper Burdigalian because of constant siliciclastic inputs and deepening of the Bonifacio straight.  相似文献