The Cause of Breaks in Holocene Beach Ridge Progradation at Bengello Beach

The data that was collected for this thesis includes thermoluminescent dates, topographic surveys using a Sokkia total station, mapped stratigraphic changes sourced from the use of ground-penetrating radar (GPR), LiDAR, vegetation analyses, contemporary analogue comparison and bruun model testing, across five transects at Bengello Beach, NSW. The data was collected between 2007 and 2010. The date range of the beach ridge plain was to approximately 6000 cal BP. The data was used to identify periods of erosion and assess changes in sea level and wave climate throughout the late Holocene.

本论文采集的数据集涵盖了澳大利亚新南威尔士州本杰洛海滩（Bengello Beach, NSW）5条断面的多类数据：热释光测年数据、采用索佳（Sokkia）全站仪开展的地形测量数据、基于探地雷达（ground-penetrating radar, GPR）与激光雷达（LiDAR）获取的地层变化制图数据、植被分析结果、现代类比对比结果以及布鲁恩模型（bruun model）测试结果。该数据集的采集时间为2007年至2010年。该海滩脊平原的年代跨度约为6000 cal BP（距今校准年）。本数据集被用于识别全新世晚期的侵蚀时段，并评估该时期的海平面与波浪气候演变情况。