首页> 外文期刊>Journal of Volcanology and Geothermal Research >The Proximal Marine Record Of Somma-vesuvius Volcanic Activity In The Naples And Salerno Bays, Eastern Tyrrhenian Sea, During The Last 3 Kyrs
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The Proximal Marine Record Of Somma-vesuvius Volcanic Activity In The Naples And Salerno Bays, Eastern Tyrrhenian Sea, During The Last 3 Kyrs

机译:最近3年内,东第勒尼安海那不勒斯和萨莱诺湾的索马维苏威火山活动的近端海洋记录

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The tephrostratigraphic analysis of nine gravity cores acquired on the continental shelf of the Naples and Salerno bays documents the proximal record of Somma-Vesuvius volcanic activity during the latest Holocene (last 3 kyrs). Five tephra layers from southern Naples Bay and three tephra layers from northern Salerno Bay were recognised in cores and their sedimentologic structures, textural parameters, stratigraphy and major and trace-element composition described. Proximal products of the well known 79 A.D. eruption along with those of the interplinian activity at 2.7 ka B.P., were identified both in the southern Naples Bay and in the northern Salerno Bay. They represent excellent marker horizons interbedded within the Late Holocene marine record. In addition, several radiocarbon datings provided age constraints on a number of tephras overlaying the 79 A.D. deposits and allowed a detailed stratigraphic reconstruction of medieval (1137 A.D.-685 A.D.) and more recent eruptions as recorded for the first time at sea. These results integrate previous research carried out on subaerial deposits providing new insights on the dispersion, deposition and grain-size distributions, along the northern Campania coastal zone, of recent Somma-Vesuvius products, some of which are still poorly known. The tephrostratigraphic approach to the study of marine sequences of proximal and adjacent areas can thus provide a more detailed description of physical characteristics of pyroclastic deposits, necessary for the correct assessment of volcanic hazard in the area.
机译:对那不勒斯和萨勒诺海湾大陆架上采集的9个重力岩心的岩相地层学分析记录了最近全新世(最后3个基尔)期间索马-维苏威火山活动的近端记录。在岩心中识别出了来自那不勒斯湾南部的五层红喉层和来自萨勒诺湾北部的三层红喉层,并描述了它们的沉积学结构,质地参数,地层以及主要和微量元素组成。在那不勒斯湾南部和萨勒诺湾北部都发现了公元79年喷发的近端产物和2.7 ka B.P的夹层间活动的近端产物。它们代表了晚全新世海相记录中嵌入的极好的标记层。此外,几次放射性碳测年提供了对覆盖公元79年沉积物的许多特弗拉斯的年龄限制,并允许对中世纪(公元1137年-685年)进行详细的地层重建,并首次在海上记录到最近的火山喷发。这些结果整合了先前对地下沉积物进行的研究,从而提供了有关最近的Somma-Vesuvius产品沿坎帕尼亚北部沿海地区的分散,沉积和粒度分布的新见解,其中有些仍然鲜为人知。因此,用断层地层学方法研究近端和邻近地区的海洋层序,可以更详细地描述火山碎屑沉积物的物理特征,这对于正确评估该地区的火山危害是必不可少的。

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