首页> 外文期刊>Journal of Volcanology and Geothermal Research2012V243-244NOCT,15 >Post-collapse evolution of a coastal caldera system: Insights from a 3D multichannel seismic survey from the Campi Flegrei caldera (Italy)
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Post-collapse evolution of a coastal caldera system: Insights from a 3D multichannel seismic survey from the Campi Flegrei caldera (Italy)

机译:沿海破火山口系统崩溃后的演变:来自Campi Flegrei破火山口(意大利)的3D多通道地震勘测的见解

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摘要

In this study we present the first 3D high-resolution multichannel seismic dataset from a (partly) submerged caldera setting, the Campi Flegrei caldera (CFc). Our work aims at examining the spatial and temporal evolution of the CFc since the last caldera-forming event, the Neapolitan Yellow Tuff (NYT, 15 ka) eruption. The main objectives are to investigate the caldera's shallow (<200 m) subsurface structure and post-NYT-collapse (<15 ka) deformational processes, the manifestation of magmatic and hydrothermal processes in the subsurface, as well as the volume, dispersal and explosivity of coastal post-collapse eruptions, thereby significantly advancing our current knowledge of the CFc.
机译:在这项研究中,我们展示了来自(部分)淹没破火山口环境的第一个3D高分辨率多通道地震数据集,即Campi Flegrei破火山口(CFc)。我们的工作旨在检查自上一次火山口形成事件那不勒斯黄凝灰岩(NYT,15 ka)喷发以来,CFc的时空演变。主要目的是研究破火山口的浅层(<200 m)地下结构和NYT塌陷后(<15 ka)变形过程,地下岩浆和热液过程的表现以及体积,扩散和爆炸性沿海崩塌后火山喷发的发生,从而大大提高了我们目前对CFc的了解。

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