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Application of 3D fine seismic interpretation technique in Dawangzhuang Area, Bohai Bay Basin, Northeast China

机译:3D精细地震解释技术在中国东北渤海湾盆地大王庄地区的应用

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摘要

One of the major problems in subsurface seismic acquisition, procession, and exploration we are facing today is the uncertainty in geologic interpretation because of the complexity of subsurface geology and the limited dimension of the subsurface data available (including drilling data, well logging, and core samples). Case studies from worldwide exploration projects indicate that an integrated, three-dimensional seismic volume visualization and interpretation workflow contributes greatly to resolving the problems we mentioned by extracting critical geologic information from within 3D seismic datasets. Over the last decade, with the increasing employment and improvement of geophysical technology and following 3D seismic data acquisition and processing, the subsurface seismic interpretation workflow is composed geological data in the study area. Finally, we finished the fine interpretation of 3D seismic data and achieved a series of success and good application results. The evolution of tectonics resulted in sub-tectonic units containing the sequences of Ek, Es, Ed, Ng, and Nm. Interpretation reveals that tectonic transition zone which controlled the evolution of the sequences because of its strength, and also, the structural pattern resulted in types of fault (such as "Y" type). The seismic interpretations provide new information on subsurface geology, including the recognition of complex structural patterns in rift lacustrine basin and the presence of a tectonic transition zone at the structural center. The interpretation of these seismic reflection profiles provides new insights into the structure, geological evolution, and petroleum potential of the study area.
机译:今天我们面临的地下地震采集,处理和勘探的主要问题之一是地质解释的不确定性,这是由于地下地质的复杂性以及可用的地下数据(包括钻探数据,测井和岩心)的维数有限的缘故样本)。来自全球勘探项目的案例研究表明,集成的三维地震体可视化和解释工作流程通过从3D地震数据集中提取关键地质信息,极大地解决了我们提到的问题。在过去的十年中,随着地球物理技术的使用和改进,以及3D地震数据的采集和处理,地下地震解释工作流程由研究区域的地质数据组成。最后,我们对3D地震数据进行了精细的解释,取得了一系列成功和良好的应用效果。构造学的演变导致亚构造单元包含了Ek,Es,Ed,Ng和Nm的序列。解释表明,构造过渡带由于其强度而控制着序列的演化,而且构造模式也导致了断层的类型(例如“ Y”型)。地震解释为地下地质提供了新的信息,包括识别裂谷湖盆中复杂的结构模式以及在结构中心存在构造过渡带。这些地震反射剖面的解释为研究区域的结构,地质演化和石油潜力提供了新的见解。

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