中更新世期间意大利中南部的爆炸性火山活动:从阿切尔诺盆地的凝灰岩层说起

IF 2.9 Q2 GEOGRAPHY, PHYSICAL Quaternary Science Advances Pub Date : 2024-04-04 DOI:10.1016/j.qsa.2024.100186
C. Pelullo , I. Arienzo , M. D’Antonio , B. Giaccio , R.S. Iovine , N. Leicher , D.M. Palladino , M. Petrelli , P. Petrosino , E. Russo Ermolli , G. Sottili , F. Totaro , G. Zanchetta
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引用次数: 0

摘要

位于意大利亚平宁半岛南部的构造古湖泊 Acerno 盆地的岩芯演替是意大利第四纪火山地层网络的一个关键点。从该盆地湖泊沉积物中的 21 个火山口岩层(年代介于 570 至 470 ka 之间)中获取了块状岩石、玻璃状基质和分离矿物(长石和辉石表晶)的微量元素和同位素(87Sr/86Sr 和 143Nd/144Nd)数据。已有的主要元素成分在这里与新获得的数据相结合。整个数据集提供了对这些块屑的全面地球化学特征描述,加强并改进了之前确定其火山源和潜在相关性的尝试。在这种情况下,以前提出的几种远端档案之间的相关性在这里得到了证实。地球化学指纹突出表明,保存在阿切尔诺湖相演替中的火山记录可归因于罗卡蒙菲纳岛、科利阿尔巴尼岛、萨巴蒂尼岛、庞蒂安岛(意大利中部拉齐奥地区)和那不勒斯火山区(意大利南部坎帕尼亚地区)的火山爆发活动,这为增进目前对意大利中更新世火山记录的了解提供了新的见解。此外,火山碎屑的归属表明,这些火山在第四纪期间的喷发活动仍不为人知。从这个角度来看,我们的研究证明了即使在很短的时间间隔内精确关联不同地质档案是多么困难。造成这种困难的原因是,大量火山活动集中在一个相对较短的时间跨度内,其产物具有相似的化学成分,而且对近距离露头的演替特征描述不完整。要彻底重建这些火山群的喷发历史,需要对远端档案进行更广泛、更深入的研究,同时对近端地区进行进一步调查。
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Explosive volcanic activity in Central-Southern Italy during Middle Pleistocene: A tale from tephra layers of the Acerno basin

The cored succession of the Acerno basin, a tectonic palaeolake located in the southern Apennines (Italy), represents a key point of the Italian tephrostratigraphic network for the Quaternary. Trace element and isotope (87Sr/86Sr and 143Nd/144Nd) data have been acquired on bulk rock, glassy groundmass and separated minerals (feldspar and pyroxene phenocrysts) from twenty-one tephra layers, dated between ∼570 and 470 ka, embedded in the lacustrine sediments of the basin. The already available major element compositions have been here combined with the newly acquired data. The whole dataset provides a full geochemical characterization of the tephra that strengthens and improves previous attempts to identify their volcanic sources and potential correlatives. In this context, several previously proposed correlations among distal archives have been here confuted. The geochemical fingerprints highlight that the volcanic record preserved in the Acerno lacustrine succession can be attributed to the explosive activity of the Roccamonfina, Colli Albani, Sabatini, Pontian islands (Latium region, Central Italy) and the Neapolitan Volcanic Area (Campania region, South Italy), providing new insights to enhance the current knowledge on the Middle Pleistocene volcanic record in Italy. Moreover, tephra attributions suggest still unknown eruptive activity of such volcanoes during the Quaternary. From this perspective, our study testifies how difficult it is to precisely correlate different geological archives even in a very short time interval. Such a difficulty arises from a large number of volcanic events concentrated in a relatively short time span, with products of similar chemical composition, and from the incomplete characterization of the successions in proximal outcrops. A thorough reconstruction of the eruptive history of these volcanic complexes requires a wider and denser study of distal archives, alongside further investigations in proximal areas.

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来源期刊
Quaternary Science Advances
Quaternary Science Advances Earth and Planetary Sciences-Earth-Surface Processes
CiteScore
4.00
自引率
13.30%
发文量
16
审稿时长
61 days
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