地震成像在海洋考古遗址调查中的潜力

T. Missiaen
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引用次数: 6

摘要

在过去的几十年里,海洋声学技术已经成为一种成功的考古研究工具,通常集中在近岸地区。最常用的技术包括侧面扫描声纳和多波束系统,旨在识别躺在海底的考古文物。然而,这些技术的主要缺点是它们不能穿透地下。海洋地震方法由于其穿透能力,可以对水下考古物体进行探测和成像。极高和超高分辨率的稳步发展使地震技术成为特定地点考古研究的重要资产。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The potential of seismic imaging in marine archaeological site investigations
Introduction Over the last decades marine acoustic techniques have become a successful investigation tool in archaeological studies, often focused on nearshore areas. The most commonly applied techniques involve side-scan sonar and multibeam systems, aimed to identify archaeological artefacts lying on the seabed. However, the main disadvantage of those techniques is that they cannot penetrate the subsurface. The marine seismic method, due to its penetration capacity, allows the detection and imaging of submerged archaeological objects. The steady development towards very high and ultra-high resolutions2 has made the seismic technique a major asset in site-specific archaeological research.
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