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Revised modelling of the post-AD 79 volcanic deposits of Somma-Vesuvius to reconstruct the pre-AD 79 topography of the Sarno River plain (Italy)

机译:修改了索马-维苏威火山的公元79年后火山岩沉积模型,以重建萨尔诺河平原(意大利)的公元79年以前的地形

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摘要

In this study the methodology proposed by Vogel & Marker (2010) to reconstruct the pre-AD 79 topography and paleo-environmental features of the Sarno River plain (Italy) was considerably revised and improved. The methodology is based on an extensive dataset of stratigraphical information from the entire Sarno River plain, a high-resolution present-day digital elevation model (DEM) and a classification and regression tree approach. The dataset was re-evaluated and 32 additional stratigraphical drillings were collected in areas that were not or insufficiently covered by previous stratigraphic data. Altogether, an assemblage of 1,840 drillings, containing information about the depth from the present-day surface to the pre-AD 79 paleo-surface (thickness of post-AD 79 deposits) and the character of the pre-AD 79 paleo-layer of the Sarno River plain was utilized. Moreover, an improved preprocessing of the input parameters attained a distinct progress in model performance in comparison to the previous model of Vogel & Marker (2010). Subsequently, a spatial model of the post-AD 79 deposits was generated. The modelled deposits were then used to reconstruct the pre-AD 79 topography of the Sarno River plain. Moreover, paleo-environmental and paleo-geomorphological features such as the paleo-coastline, the paleo-Sarno River and its floodplain, alluvial fans near the Tyrrhenian coast as well as abrasion terraces of historical and protohistorical coastlines were identified. This reconstruction represents a qualitative improvement of the previous work by Vogel & Marker (2010).
机译:在这项研究中,Vogel&Marker(2010)提出的重建萨诺河平原(意大利)AD 79之前的地形和古环境特征的方法得到了相当大的修改和改进。该方法基于整个萨尔诺河平原的地层信息的广泛数据集,高分辨率的当今数字高程模型(DEM)以及分类和回归树方法。重新评估了数据集,并在以前的地层数据没有覆盖或不足的地区收集了32次额外的地层钻探。总共进行了1,840次钻探,包括有关从现今地表到公元79年以前的古表层的深度(公元79年以后的沉积物的厚度)以及公元79年以前的古层特征的信息。萨诺河平原被利用。此外,与Vogel&Marker(2010)的先前模型相比,改进的输入参数预处理在模型性能方面获得了明显的进步。随后,生成了AD 79后沉积物的空间模型。然后将模拟的沉积物用于重建萨尔诺河平原的公元79年以前的地形。此外,还确定了古环境和古地貌特征,例如古海岸线,古萨尔诺河及其泛滥平原,第勒尼安海岸附近的冲积扇以及历史和原始历史海岸线的磨损带。这种重建代表了Vogel&Marker(2010)先前工作的质的改进。

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