首页> 外文会议>2005 SPE annual technical conference and exhibition (ATCE 2005) >Interpreting the Depositional Facies of the Upper Gharif Fluvial System UsingOil-Based Mud Images: A Case Study in Central Oman
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Interpreting the Depositional Facies of the Upper Gharif Fluvial System UsingOil-Based Mud Images: A Case Study in Central Oman

机译:基于油基泥浆图像的上盖利夫河流相沉积相解释:以阿曼中部为例

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During the early stages of developing Oman's A field, water-basedrnmud (WBM) was used to drill all wells. With this mudrnsystem the wells suffered borehole stability problems,rnespecially in the friable paleosols (fossil soils) of the Gharifrnformation. One of the advantages of drilling with WBM wasrnthe ability to run high-resolution microresistivity images.rnIn the second development stage of the field, oil-basedrnmud (OBM) was used in order to reduce the severe boreholernwashouts. However, the benefits of microresistivity boreholernimages were lost.rnWith the development of the oil-based mud imager toolrnand its deployment in the A field, key geological andrnpetrophysical information is provided for further successfulrnfield development.rnThis paper explains a new methodology for geologicallyrnevaluating the complex upper part of the Gharif formation byrnintroducing integrated data from different sources. Using thernelectrical oil-based mud images integrated with acousticrnimages, core data and openhole logs, the facies distributionrnand typing of the Permian Gharif fluvial system are interpretedrnover the field.rnNine depositional facies were identified using the oil-basedrnmud images: sand channel, heterolithic channel, abandonedrnchannel, splay/chute, debris flow/sand flat, floodplain/swamp,rntidal flat/intertidal, marine shales, and shallow marinernlimestone facies.rnThe Upper Gharif stratigraphic interval is subdivided intornchannel belts separated by thick floodplain shales. Thernpaleocurrent analysis based on these subdivisions illustratesrnthat, in the Upper Gharif, the large spectrum of trendsrnobserved for some layers is the result of deposition withrnalmost no accommodation space (meandering channel),rnwhereas other layers show clearer trends indicating possible deposition under higher energy (stream channel type). Thernvalue of the oil-based images has been its ability to delineaternthe channel belt trends and sand prediction for infill drilling.rnThe identification of these facies and their trends is criticalrnfor reservoir evaluation and in field development. However,rnrecent infill drilling results in the Upper Gharif show that sandrnprediction remains the key challenge to successfulrndevelopment.
机译:在开发阿曼A油田的早期阶段,使用了水基泥浆(WBM)来钻探所有井。有了这种泥浆系统,这些井就遇到了井壁稳定性问题,特别是在加里富纳组的易碎古土壤(化石土壤)中。使用WBM进行钻探的优点之一是能够运行高分辨率的微电阻率图像。在该领域的第二个开发阶段,使用了油基泥浆(OBM)来减少严重的井壁冲刷。但是,随着微电阻率岩心成像技术的发展,人们已经失去了这种优势。随着油基泥浆成像仪工具的发展以及在A油田的部署,为进一步成功开发油田提供了关键的地质和岩石物理信息。通过引入来自不同来源的综合数据来形成Gharif地层的一部分。利用结合了声波图像,岩心数据和裸眼测井的基于电的油基泥浆图像,解释了该地区的二叠纪Gharif河流系统的相分布和类型。使用油基的泥浆图像识别出了九个沉积相:砂岩通道,异质通道,废弃的河道,张开/溜槽,泥石流/沙地,洪泛区/沼泽,潮汐带/潮间带,海相页岩和浅层海相石灰岩相。上加里夫地层间隔细分为由厚的洪泛区页岩分隔的河道带。基于这些细分的古流分析表明,在上加里夫地区,某些层的大趋势趋势是沉积的结果,几乎没有容纳空间(蜿蜒通道),而其他层则显示出更清晰的趋势,表明在较高能量下可能沉积(流通道)。类型)。油基图像的价值在于其能够描绘出通道带趋势和预测充填钻探的砂岩的能力。这些相及其趋势的识别对于储层评估和油田开发至关重要。但是,最近在上加里夫(Gharif)进行的填充钻探结果表明,砂岩预测仍然是成功开发的关键挑战。

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