刘刚,金鼎坚,吴芳,等. 机载激光雷达在水下地貌识别与断裂构造精细解译中的应用[J]. 海洋地质与第四纪地质,2022,42(2): 190-199. doi: 10.16562/j.cnki.0256-1492.2021061502
引用本文: 刘刚,金鼎坚,吴芳,等. 机载激光雷达在水下地貌识别与断裂构造精细解译中的应用[J]. 海洋地质与第四纪地质,2022,42(2): 190-199. doi: 10.16562/j.cnki.0256-1492.2021061502
LIU Gang,JIN Dingjian,WU Fang,et al. Application of airborne LiDAR to identification of underwater geomorphology and fine interpretation of faults.[J]. Marine Geology & Quaternary Geology,2022,42(2):190-199. doi: 10.16562/j.cnki.0256-1492.2021061502
Citation: LIU Gang,JIN Dingjian,WU Fang,et al. Application of airborne LiDAR to identification of underwater geomorphology and fine interpretation of faults.[J]. Marine Geology & Quaternary Geology,2022,42(2):190-199. doi: 10.16562/j.cnki.0256-1492.2021061502

机载激光雷达在水下地貌识别与断裂构造精细解译中的应用

Application of airborne LiDAR to identification of underwater geomorphology and fine interpretation of faults.

  • 摘要: 机载激光雷达水深测量是高效获取高精度近岸海底地形的一种新型技术,具有测量精度高、效率高、作业区域广的特点。通过分析CZMIL Nova Ⅱ机载激光雷达测深系统获取的南海某岛高分辨率海底地形数据,发现除地貌类型的识别以外,该数据还可用于海底断裂构造的高精度解译。通过对激光雷达测深渲染图像的解译,发现工作区海底地貌由沙嘴、海岬、海湾、古波切台、岸坡、断陷洼地、峡谷、平原和断块残丘组成;海底发育走向NW、NNW、NNE和NEE的 4组主要断裂,环绕海岛的岸线和水下地貌受多组断裂的控制;海底断裂系统在地表的延伸部分得到了CZMIL Nova Ⅱ系统数字相机同步拍摄的陆地高分辨率图像的验证。本项研究将陆地构造的遥感解译方法拓展到高程渲染图像的水下断裂解译,在清澈水域的海岸带调查工作中具有很大的应用潜力。

     

    Abstract: The airborne lidar bathymetry (ALB) is a new equipment for efficient survey of offshore seabed topography with high precision, high accuracy, high efficiency and wide operation area. By study of the high-resolution submarine topography data collected by the CZMIL Nova Ⅱ ALB system from an island in the South China Sea, it is found that the data can be used for efficient identification of geomorphic types and precise interpretation of submarine fractures, and the principles and methods adopted are very similar to the remote sensing interpretation for land structures. Through the detailed interpretation of the images acquired by lidar sounding, many seabed geomorphic types are found in the study area, for examples, the sand spit, headland, bay, ancient wave-cut platform, bank slope, fault depression, valley, submarine plain and residual fault block. The submarine landform and coastline surrounding the island are mainly controlled by fractures. Four groups of faults in NW, NNW, NNE and NEE directions are found on the seafloor, basically in consistent with the regional tectonic patterns. The extension of submarine rift system on land surface is proved by the high-resolution images acquired synchronously by the digital camera of CZMIL Nova Ⅱ system. Our experience in this survey proves that to extend the technique of remote sensing interpretation for land structures to the underwater fault interpretation offshore is a good solution to the precise detection of fault structures in coastal shallow waters.

     

/

返回文章
返回