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Architectural elements in a high-continuity sand-prone turbidite system, late Precambrian Kongsfjord Formation, northern Norway: Application to hydrocarbon reservoir characterization

机译:挪威北部前寒武纪Kongsfjord组晚期高连续性易发生砂质浊积岩体系中的建筑元素:在油气藏表征中的应用

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Quantifying the geometry of high-continuity (relatively unconfined) sand-prone systems in deep-water sedimentary environments is important both for a better understanding of the intrinsic nature of these systems(volumetrics, stacking patterns, etc.) and for the potential application of this data to modeling the depositional characteristics of such systems for basin analysis and reservoir modeling. A quantitative methodology is presented for defining the geometry of architectural elements within sedimentary systems. This methodology is then applied to a detailed analysis of sand-rich, deep-water systems, with examples from the late Precambrian Kongsfjord Formation, Arctic Norway, and other published outcrop and subsurface data. The efficacy of the scheme is demonstrated by its ability to discriminate effectively between reservoir architectural elements of differing scales within environments (e.g., individual beds, packets of beds) and also between environments (e.g., abyssal plain outerfan lobe, and submarine channel deposits). This scheme permits a quantitative, more objective means of comparing modern and ancient, including subsurface, depositional systems. The methodology and analysis presented here provide important geometrical and geological information on architectural elements at the subseismic, typical interwell scale. The data produced by this methodology should prove useful for reservoir production and development techniques. This methodology also should have applicability in exploration, through its application to architectural elements at the fan and basin scale. In exploration and production in deep-water clastic systems, the available data, which are commonly extremely expensive to collect, typically consist of seismic data (with high aerial but relatively poor vertical resolution) and generally few wells (with high vertical resolution but extremely low aerial resolution). Therefore, information derived from suitable outcrop analogs on the geometry of fan elements augments significantly the typically sparse available industry data from exploration and production.
机译:量化深水沉积环境中高连续性(相对不受限制)的易发生砂土的系统的几何形状,对于更好地理解这些系统的内在本质(体积,堆积模式等)以及潜在应用具有重要意义。这些数据可以对这类系统的沉积特征进行建模,以进行盆地分析和储层建模。提出了一种定量方法,用于定义沉积系统内建筑元素的几何形状。然后,将该方法应用于富含砂的深水系统的详细分析,并以前寒武纪Kongsfjord组,挪威北极以及其他已公开露头和地下数据为例。该方案的有效性通过有效区分环境中不同尺度的储层建筑元素(例如单个床,床包)以及环境之间(例如深海平原外扇叶和海底河道沉积物)的能力证明。此方案允许比较现代和古代(包括地下,沉积系统)的定量,更客观的手段。本文介绍的方法和分析以亚地震的典型井间尺度提供了有关建筑元素的重要几何和地质信息。这种方法产生的数据应证明对油藏生产和开发技术有用。通过将这种方法应用于风扇和盆地尺度的建筑元素,该方法也应具有勘探应用性。在深水碎屑系统的勘探和生产中,通常收集起来非常昂贵的可用数据通常包括地震数据(具有较高的空中但垂直分辨率相对较低)和少量的井(具有较高的垂直分辨率但非常低的井)空中分辨率)。因此,从合适的露头类似物获得的有关风扇元件几何形状的信息大大增加了勘探和生产中通常稀疏的可用行业数据。

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