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Case history high-resolution, deep-towed, multichannel seismic survey of deep-sea gas hydrates off western Canada

机译:案例历史记录对加拿大西部深海天然气水合物进行高分辨率,拖曳,多通道地震调查

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A multichannel seismic survey was carried out us- ing the high-resolution deep-towed acoustics/geophysics system(DTAGS)to image the structure of deep-sea gas hydrates on the continental slope off Vancouver Island and to determine the velocity profile of the hydrated sediments. The high-frequency DTAGS data provide the means to estimate the frequency response of the bottom simulating reflector(BSR)that defines the base of the hydrate stability field in these sediments, over a broad frequency band from 15 to 650 Hz. The DTAGS sections resolved fine-scale layering as thin as a few meters within the hydrated zone and below the BSR, and they revealed small-scale faults and vertically oriented zones of very low acoustic reflectivity that may represent channels for upward migration of fluids or gas.
机译:利用高分辨率的深层拖曳声波/地球物理系统(DTAGS)进行了多通道地震勘测,以对温哥华岛外陆坡上的深海天然气水合物的结构进行成像,并确定水合物的速度分布。沉积物。高频DTAGS数据提供了一种手段,可用来估计底部模拟反射器(BSR)的频率响应,该频率响应在15至650 Hz的宽频带内定义了这些沉积物中水合物稳定性场的基础。 DTAGS断层解析了水化区内和BSR下方几米薄的细尺度分层,它们揭示了小规模的断层和垂直反射带,其声反射率极低,可能代表了流体或气体向上迁移的通道。

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