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Bathymetry of the Adriatic Sea: The legacy of the last eustatic cycle and the impact of modern sediment dispersal

机译:亚得里亚海的测深法:最后一次欣喜循环的遗留物和现代沉积物扩散的影响

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The Istituto di Scienze Marine (ISMAR-CNR) has conducted several research projects on the Italian side of the Adriatic Sea over more than 15 years, collecting bathymetric, geophysical and sediment core data to perform multidisciplinary studies of modern sediment dynamics and of past environmental changes during the last eustatic cycle. A crucial step in this direction was the construction of a detailed bathymetry, a time-consuming task due to the extensive shallow water portion of the basin. Given the setting of the Adriatic Sea and the long-lasting research effort, the bathymetric map is necessarily based on heterogeneous data with uneven spatial distribution of Single-Beam echo-soundings. The main objective of this work is to illustrate the methodology applied to compile the bathymetric map of the west side of the Adriatic Sea at basin scale (1:750,000) and to describe the main morphological units that characterise the seafloor and reflect its main geological features. This bathymetry can also be used in oceanographic modelling both at regional and local scale, focussing on the interaction between bottom currents and seafloor morphology.
机译:科学海洋研究所(ISMAR-CNR)在亚得里亚海的意大利一侧进行了超过15年的几个研究项目,收集了水深,地球物理和沉积物核心数据,以对现代沉积物动力学和过去的环境变化进行多学科研究。在最后一次欣喜循环中。朝这个方向迈出的关键一步是建立详细的测深图,由于盆地浅水区很大,这是一项费时的工作。考虑到亚得里亚海的环境和长期的研究努力,测深图必定基于异质数据,且单波束回声的空间分布不均匀。这项工作的主要目的是说明用于编制流域尺度(1:750,000)的亚得里亚海西侧水深图的方法,并描述表征海底并反映其主要地质特征的主要形态单位。 。这种测深法还可以用于区域和局部尺度的海洋学建模,重点在于底流和海底形态之间的相互作用。

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