Data processing of hydroacoustic data as support to mapping and characterization of seafloor

Giankarlo R. F. Fernandes de Oliveir, M. L. S. Nogueira, H. Vital, Josibel Gomes de Oliveira Junior
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Abstract

This work aims to present a processing flow designed for shallow seismic data acquired in the northern continental shelf of Rio Grande do Norte State, adjacent to Areia Branca city. This area was choose because of the presence of an important incised-valley system, between depths of 15 m to 25m. The understanding of the formation and cenozoic filling of incised valleys has contributed more and more to studies with similar reservoirs of oil and gas. The data were acquired with a sub-bottom profiler type chirp, using small boats. The signal penetration reached approximately 45m with subsurface water depths of up to 40m. During activities were acquired information of parameterization software acquisition, software and processing tools. All data were integrated with GIS (Geographic Information Systems). Processing consisted in the adaptation of coordinate system, spectral analysis, optimization of the process of removing the water depth, application of low-pass filters and FK, according to the need of each section and bathymetric correction. The results revealed a smoothing effect of the waves, noise attenuation and multiple best contrasting the different types of reflectors thus enabling the identification of different seism facies in existing sections.
水声数据的数据处理为海底制图和表征提供支持
这项工作旨在为北里奥格兰德州北部大陆架获取的浅层地震数据提供一种处理流程,该大陆架毗邻Areia Branca市。之所以选择这个地区,是因为这里有一个重要的切割山谷系统,深度在15米到25米之间。对断陷谷的形成和新生代充填的认识,对类似油气储层的研究贡献越来越大。数据是用小船用海底剖面仪式啁啾获取的。信号穿透深度约45m,地下水深达40m。活动期间获取了参数化、软件获取、软件和加工工具等信息。所有数据均与GIS(地理信息系统)集成。处理包括坐标系的适应、光谱分析、去除水深过程的优化、低通滤波器和FK的应用,并根据各剖面的需要进行水深校正。结果表明,不同类型反射波具有平滑、噪声衰减和多重最佳对比的效果,从而可以在现有剖面中识别不同的地震相。
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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