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DOI | 10.1007/s00531-020-01933-6 |
Geochemical and Sr–Nd isotopic features of the Zaro volcanic complex: insights on the magmatic processes triggering a small-scale prehistoric eruption at Ischia island (south Italy) | |
Pelullo C.; Cirillo G.; Iovine R.S.; Arienzo I.; Aulinas M.; Pappalardo L.; Petrosino P.; Fernandez-Turiel J.L.; D’Antonio M. | |
发表日期 | 2020 |
ISSN | 14373254 |
起始页码 | 2829 |
结束页码 | 2849 |
卷号 | 109期号:8 |
英文摘要 | The prehistoric (< 7 ka) Zaro eruption at Ischia island (Southern Italy) produced a lava complex overlaying a pyroclastic deposit. Although being of low energy, the Zaro eruption might have caused casualties among the neolithic population that inhabited that area of Ischia, and damages to their settlements. A similar eruption at Ischia with its present-day population would turn into a disaster. Therefore, understanding the magmatic processes that triggered the Zaro eruption would be important for volcanic hazard assessment and risk mitigation, so as to improve a knowledge that can be applied to other active volcanic areas worldwide. The main Zaro lava body is trachyte and hosts abundant mafic and felsic enclaves. Here all juvenile facies have been fully characterized from petrographic, geochemical and isotopic viewpoints. The whole dataset (major and trace element contents; Sr–Nd isotopic composition) leads to rule out a genetic link by fractional crystallization among the variable facies. Thus, we suggest that the Zaro mafic enclaves could represent a deep-origin mafic magma that mingled/mixed with the main trachytic one residing in the Ischia shallow magmatic system. The intrusion of such a mafic magma into a shallow reservoir filled by partly crystallized, evolved magma could have destabilized the magmatic system presumably acting as a rapid eruption trigger. The resulting processes of convection, mixing and rejuvenation have possibly played an important role in pre- and syn-eruptive phases also in several eruptions of different sizes in the Neapolitan area and elsewhere in the world. © 2020, The Author(s). |
英文关键词 | Ischia island; Isotope geochemistry; Mafic enclaves; Mineral chemistry; Zaro volcanic complex |
语种 | 英语 |
scopus关键词 | igneous geochemistry; inclusion; lava; magmatism; neodymium isotope; prehistoric; strontium isotope; trigger mechanism; volcanic eruption; Campania [Italy]; Ischia; Italy; Napoli [Campania] |
来源期刊 | International Journal of Earth Sciences
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/147597 |
作者单位 | Dipartimento di Scienze della Terra, dell’Ambiente e delle Risorse, Università Degli Studi di Napoli Federico II, Naples, Italy; Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Napoli Osservatorio Vesuviano, Naples, Italy; Departament de Mineralogia, Petrologia i Geologia Aplicada, Facultat de Ciències de la Terra, Universitat de Barcelona, c/ Martí Franquès s/n, Barcelona, 08028, Spain; Geosciences Barcelona, GEO3BCN, CSIC, Lluís Solé i Sabaris s/n, Barcelona, 08028, Spain |
推荐引用方式 GB/T 7714 | Pelullo C.,Cirillo G.,Iovine R.S.,等. Geochemical and Sr–Nd isotopic features of the Zaro volcanic complex: insights on the magmatic processes triggering a small-scale prehistoric eruption at Ischia island (south Italy)[J],2020,109(8). |
APA | Pelullo C..,Cirillo G..,Iovine R.S..,Arienzo I..,Aulinas M..,...&D’Antonio M..(2020).Geochemical and Sr–Nd isotopic features of the Zaro volcanic complex: insights on the magmatic processes triggering a small-scale prehistoric eruption at Ischia island (south Italy).International Journal of Earth Sciences,109(8). |
MLA | Pelullo C.,et al."Geochemical and Sr–Nd isotopic features of the Zaro volcanic complex: insights on the magmatic processes triggering a small-scale prehistoric eruption at Ischia island (south Italy)".International Journal of Earth Sciences 109.8(2020). |
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