Kamaruzaman Erman H, La Croix Andrew D, Kamp Peter J J
Sedimentary Environments and Analogues Research Group, Earth and Environmental Sciences, School of Science, University of Waikato, Private Bag 3105, Hamilton 3240, New Zealand.
Data Brief. 2024 Jan 9;52:110035. doi: 10.1016/j.dib.2024.110035. eCollection 2024 Feb.
The aim of constructing 3D computer models of outcrops of the Mount Messenger Formation using unmanned aerial vehicle (UAV) drone technology was to enable better visualization and potential for analysis of deep-water sedimentary systems in Taranaki Basin, New Zealand. The Late Miocene-aged strata crop out along the north Taranaki coast of western North Island, New Zealand. The Mount Messenger Formation sandstone and siltstone beds are outstanding examples of deep-water sedimentary strata. These strata can be observed in outcrop sections, as well as in offshore drillholes (wireline logs) and in seismic reflection data acquired immediately offshore of the north Taranaki coastal section. In previous research undertaken on the Mount Messenger Formation in North Taranaki Basin, geologists used photographs and coupled these with observations and descriptions of strata in the field. Modern UAV drone technology now enables 3D perspectives to be obtained of outcrop sections, which greatly improves geometrical analysis of the rocks. This type of analysis, coupled with mapping of seismic reflection data in the immediate offshore area has enabled us to better understand the nature of Mount Messenger Formation deep-water sedimentary strata and to interpret the associated paleogeography with implications for energy resource exploration and evaluation. Using UAV drone photogrammetry, we acquired ∼3000 images of the Mount Messenger Formation outcrop at four locations along the north Taranaki coast. Drone surveys were conducted using a real-time kinetic (RTK) global positioning system (GPS) for accurate geolocation. The surveys were conducted on a DJI Phantom 4 drone, with a focal length of 24 mm with a 20-megapixel resolution. Survey images overlapped by 80-90%. The drone work adhered to the rules and regulations of the Aviation Security Service and the University of Waikato, New Zealand. Images were captured using programmed flight paths where the drone faced the outcrops at distances ranging from ∼3-7 m. 3D computer models were constructed using Pix4Dmapper version 4.4.12 to generate dense 3D point clouds, digital surface models (DSMs), triangle meshes, and orthomosaic images of the outcrops (i.e., 3D models). Once the 3D computer models of the outcrops were constructed, they were exported out of Pix4Dmapper as ArcGIS Scene Layer Package format (.slpk) and loaded into ArcGIS Pro version 3.0.3 for further analysis. The 3D computer models comprise a rich and valuable scientific dataset that can enhance geological analysis of sedimentary strata beyond the capabilities of photographs and manual fieldwork. These models allow desktop analysis of the geology and "virtual fieldwork" by imaging areas that are commonly inaccessible on foot due to their high elevation above ground level, location in rugged and steep terrane, as well as periodic intertidal flooding. This electronic geological dataset is stored in commonly used spatial format and plain-text ASCII files, allowing the preservation of geological data in digital records, especially when the outcrops are prone to erosion and cover by vegetation. The drone model dataset can be reused by the scientific community for virtual geological fieldwork, as petroleum and water reservoir analogues, as well as for research on coastal, environmental and geotechnical topics.
利用无人机技术构建梅辛杰山组露头的三维计算机模型,目的是更好地可视化和分析新西兰塔拉纳基盆地的深水沉积系统。中新世晚期地层出露于新西兰北岛西部塔拉纳基海岸北部。梅辛杰山组的砂岩和粉砂岩层是深水沉积地层的杰出实例。这些地层可在露头剖面、近海钻孔(电缆测井)以及塔拉纳基海岸北部近海获取的地震反射数据中观察到。在之前对塔拉纳基盆地北部梅辛杰山组的研究中,地质学家使用照片,并将其与实地地层观察和描述相结合。现代无人机技术现在能够获取露头剖面的三维视角,这极大地改善了对岩石的几何分析。这种分析与近海区域地震反射数据的测绘相结合,使我们能够更好地了解梅辛杰山组深水沉积地层的性质,并解释相关的古地理情况,对能源资源勘探和评估具有重要意义。利用无人机摄影测量,我们在塔拉纳基海岸北部的四个地点获取了约3000张梅辛杰山组露头的图像。使用实时动态(RTK)全球定位系统(GPS)进行无人机测量,以实现精确的地理定位。测量使用的是大疆精灵4无人机,焦距为24毫米,分辨率为2000万像素。测量图像的重叠率为80 - 90%。无人机作业遵守了新西兰航空安全局和怀卡托大学的规章制度。使用编程飞行路径拍摄图像,无人机在距离露头约3 - 7米的范围内面对露头。使用Pix4Dmapper版本4.4.12构建三维计算机模型,以生成密集的三维点云、数字表面模型(DSM)、三角网和露头的正射镶嵌图像(即三维模型)。一旦构建了露头的三维计算机模型,就将其作为ArcGIS场景图层包格式(.slpk)从Pix4Dmapper中导出,并加载到ArcGIS Pro版本3.0.3中进行进一步分析。三维计算机模型包含丰富且有价值的科学数据集,能够加强对沉积地层的地质分析,这是照片和人工野外工作所无法实现的。这些模型允许通过对因海拔高、位于崎岖陡峭地形以及周期性潮间带洪水而通常无法徒步到达的区域进行成像,在桌面上进行地质分析和“虚拟野外工作”。这个电子地质数据集以常用的空间格式和平文本文本ASCII文件存储,可将地质数据保存在数字记录中,特别是当露头容易受到侵蚀并被植被覆盖时。无人机模型数据集可供科学界用于虚拟地质野外工作、作为石油和水库类似物,以及用于海岸、环境和岩土工程主题的研究。