Location accuracy of seabed nodes during 3D seismic survey for seep studying at Laptev sea.

D. Ilinskiy
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Abstract

Summary Recent years marine surveys have provided a large and important data for mapping gaseous emissions from the seabed (the so-called seeps) of the North Seas of Russia. A number of researchers associate these phenomena with the release of methane from buried layers of permafrost on the shelf of the Arctic seas, which can potentially change the ratio of greenhouse gases in the Arctic and affect global climate change. The several important questions on the structure, composition and nature of these phenomena still remain unresolved. One of the ways to solve the questions posed is to perform detailed 3D seismic survey of high accuracy. During the 73th scientific voyage of R/V “Akademik Mstislav Keldysh” (AMK), 3-D reconnaissance seismic survey with seabed nodes was carried out. To study the internal structure of the sedimentary cover around the mega seep, we use a 3D reflection seismic method with seabed seismic nodes. The observation template consists of 16 4-component seismic seabed nodes with 300 meters spacing in both directions. Despite the absence of differential corrections for GPS/GLONASS, the obtained positioning accuracy of nodes on the sea bottom is sufficient for carrying out 3-D seismic survey.
在拉普捷夫海进行三维地震勘测以研究渗漏时海底节点的定位精度。
摘要 近年来的海洋调查为绘制俄罗斯北海海底气体排放图(即所谓的渗漏)提供了大量重要数据。一些研究人员将这些现象与北极海域陆架上埋藏的永久冻土层释放甲烷联系起来,认为甲烷有可能改变北极地区温室气体的比例,影响全球气候变化。关于这些现象的结构、组成和性质的几个重要问题仍未得到解决。解决这些问题的方法之一是进行高精度的详细三维地震勘测。在 "Akademik Mstislav Keldysh "号考察船(AMK)第 73 次科学考察期间,进行了带有海底节点的三维勘探地震勘测。为了研究特大渗漏周围沉积覆盖层的内部结构,我们采用了带海底地震节点的三维反射地震方法。观测模板由 16 个 4 分量海底地震节点组成,双向间距 300 米。尽管没有 GPS/GLONASS 的差分校正,海底节点的定位精度仍足以进行三维地震勘测。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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