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Kumancrnada 3D seismic data acquisition and processing

机译:Kumancrnada 3D地震数据采集与处理

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In the Nankai Trough off Kii Peninsula, the first scientific drilling by D/V Chikyu commenced in September 2007 as a major component of the Integrated Ocean Drilling Program (IODP), which has been an international collaborative scientific drilling program together with 22 countries since October 2003. One of its scientific challenges is to drill through the seismogenic zone to reveal the nature and mechanism of large earthquake generation. Prior to drilling, we carried out a 2D seismic survey in 2003 to identify hazards for safe and smooth drilling operation and to obtain detailed characteristics of the accretionary prism. The 2D seismic profiles, however, have some technical limitation of imaging at some targets due to the complexities of sea floor topography and sub bottom geological structures. To extend the 2D seismic results, a high resolution 3D seismic survey was conducted by M/V Nordic Explorer (PGS) in 2006. The survey area was outside shipping lanes, and fishing activities were well managed. There was, however, a strong Kuroshio Current in the southern part of the 3D survey area which significantly affected both data acquisition and data processing. The appropriate data processing including Pre-Stack Time Migration (PSTM) was carried out by CGGAP (currently CGGVeritas). To deal with the data characteristics, the processing emphasized the following three points: swell noise attenuation, multiple reflection attenuation, and handling of irregular acquisition geometry. The seismic cube, obtained as the data processing result, shows clear images of the shallow geology and most deeper targets. The Kumano-nada 3D seismic data provided information required for the scientific drilling by D/V Chikyu, and has been providing valuable information for marine science in the area.
机译:在基伊半岛南部的南海海槽中,D / V Chikyu于2007年9月开始了首次科学钻探工作,这是综合海洋钻探计划(IODP)的主要组成部分,该计划自10月以来一直是与22个国家一起开展的国际合作科学钻探计划2003年。它的科学挑战之一是钻探成地震带,以揭示大地震发生的性质和机理。在进行钻探之前,我们于2003年进行了2D地震勘测,以识别安全平稳的钻探操作危险并获得增生棱镜的详细特性。但是,由于海床地形和海底地质结构的复杂性,二维地震剖面在某些目标成像方面存在一定的技术局限性。为了扩展2D地震结果,M / V Nordic Explorer(PGS)于2006年进行了高分辨率3D地震勘测。勘测区域位于航道之外,并且捕鱼活动得到良好管理。但是,在3D调查区域的南部,黑潮强烈,这对数据采集和数据处理都产生了重大影响。包括栈前时间迁移(PSTM)在内的适当数据处理由CGGAP(当前为CGGVeritas)进行。为了处理数据特征,该处理强调了以下三点:突波噪声衰减,多次反射衰减以及不规则采集几何的处理。作为数据处理结果获得的地震立方体显示了浅层地质和最深目标的清晰图像。 Kumano-nada 3D地震数据提供了D / V Chikyu进行科学钻探所需的信息,并一直为该地区的海洋科学提供有价值的信息。

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