首页> 外文会议>EAGE Conference Exhibition >3D Seismic Data Helps to Lift the Fog - Structural and Stratigraphic Architectural Observations of a Cretaceous Carbonate Platform, offshore Qatar, Submitted to Repeated Emersion and Fluvial Incision
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3D Seismic Data Helps to Lift the Fog - Structural and Stratigraphic Architectural Observations of a Cretaceous Carbonate Platform, offshore Qatar, Submitted to Repeated Emersion and Fluvial Incision

机译:3D地震数据有助于提升白垩纪碳酸盐盐平台,近海卡塔尔的雾结构和地层建筑观察,提交重复的发液和河流切口

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Arecent marine 3D seismic survey over Block 4, Qatar, provides outstanding images of Mid-Upper Cretaceous stratigraphic intervals and allows detailed observations of both structural and stratigraphic architecture including insights into depositional settings from seismic morphology. The top of theAptian carbonate Shuaiba Formation is a surface of regional significance subjected to exposure and erosion. Seismic data indicates incision by a through going channel system which displays incised valley morphology. From interpretation of multiple seismic derived datasets the stratigraphic architecture of the channel systems is demonstrated and the nature and origin of the channel fill discussed. The structural architecture of Turonian faulting affecting the Shuaiba surface is briefly examined along with the nature of the Turonian Unconformity forming the Middle-Upper Cretaceous Boundary. The Upper Cretaceous succession in Qatar culminates in the deposition of the Maastrichtian Simsima Formation which is capped by a significant unconformity associated with a period of renewed tectonism. Recognising the top Simsima unconformity has proved problematic in the vicinity of Block 4, but detailed seismic interpretation has identified a likely candidate. Moreover, from flattened seismic volumes and Seismic WaveformAnalysis a detailed seismic facies prediction for the Simsima is presented and the affects of syn-depositional faulting on facies distribution highlighted.
机译:由街区4,卡塔尔的共同海洋3D地震调查提供了中上层白垩纪地层间隔的出色图像,并允许对结构和地层架构的详细观察,包括从地震形态的沉积环境中的洞察。 Theaptian碳酸盐酸碱形成的顶部是对暴露和侵蚀进行的区域意义的表面。地震数据表示通过显示切口谷形态的通道系统切开。根据多次地震派生数据集的解释,证明了渠道系统的地层架构,并讨论了渠道填充的性质和起源。随着形成中上层白垩纪边界的涡轮织物不整形的性质,简要检查了影响舒邦巴表面的涡杉误差的结构架构。卡塔尔的上白垩纪连续在马斯特里亚斯米西玛的沉积中沉积,其被与一段更新的构造周期相关的显着不一致。识别顶部Simsima不整合在框4附近已经证明了问题,但详细的地震解释已经确定了可能的候选人。此外,从扁平地震作用和地震波形分析,提出了一种详细的辛西米的地震相预测,并影响了突出显示的相片分布上的同步沉积断层的影响。

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