气候变化领域集成服务门户(CCPortal): The Campi Flegrei caldera unrest: Discriminating magma intrusions from hydrothermal effects and implications for possible evolution

CCPortal

DOI	10.1016/j.earscirev.2018.11.007
	The Campi Flegrei caldera unrest: Discriminating magma intrusions from hydrothermal effects and implications for possible evolution
	Troise C.; De Natale G.; Schiavone R.; Somma R.; Moretti R.
发表日期	2019
ISSN	0012-9088
起始页码	108
结束页码	122
卷号	188
英文摘要	The Campi Flegrei caldera in Southern Italy is one of the most populated active volcanoes on Earth. It has an unprecedented record of historical unrest and eruption that dates back to 2.2 ka BP and provides key insights for understanding the dynamic evolution of large calderas. Since 1950, it has undergone four episodes of caldera-wide uplift and seismicity, which have raised the coastal town of Pozzuoli, near the centre of unrest, up to 4.5 m and triggered the repeated evacuation of some 40,000 people. After about 20 years of subsidence, following the uplift peak reached in 1984, the caldera started a new, low rate uplift episode, accompanied by low magnitude seismicity and marked geochemical changes in fumaroles. In this area it is crucial to discriminate episodes of shallow magma intrusion from hydrothermal perturbations, which are both able to generate unrest signals. In this paper, by a critical review of previous literature and some new results, we discriminate, in the unrest episodes, the relative contributions of hydrothermal effects and shallow magma intrusions. Our review is aimed also to show the different behavior of the largest unrest episodes, such as the 1982–1984, and the present, ungoing unrest characterized by smaller rate but longer lasting uplift. We show that for the former, larger uplift of the 80's, there is clear evidence for shallow magma intrusion, and we are able to compute the amount of intruded magma volume. For the present, on-going uplift, on the contrary, there is no evidence for magmatic activity at shallow depth. As a main result of our analysis, we demonstrate here the present unrest, characterized by much lower uplift rates and seismicity, is only interpretable as due to large gas fluxes coming from the deeper magma reservoir; without any appreciable contribution from shallow magma or recent magmatic intrusion. Our results shed new light on the interpretation of caldera unrest worldwide, and clearly indicate the most constraining data and the most rigorous procedures of data analysis for a correct interpretation of volcanic unrest. © 2018 The Authors
语种	英语
scopus关键词	caldera; fumarole; hydrothermal alteration; igneous intrusion; magma chamber; seismicity; tectonic evolution; uplift; volcanic eruption; volcano; Campania [Italy]; Campi Flegrei; Italy; Napoli [Campania]
来源期刊	EARTH-SCIENCE REVIEWS
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/209987
作者单位	Istituto Nazionale di Geofisica e Vulcanologia, Naples (I), Italy; Università della Campania ‘Luigi Vanvitelli’, Dipartimento di Ingegneria, Naples (I), Italy; Institute de Physique du Globe, équipe des Systèmes Volcaniques - Observatoire Volcanologique et Sismologique de Guadeloupe, Gourbeyre (FWI), France
推荐引用方式 GB/T 7714	Troise C.,De Natale G.,Schiavone R.,et al. The Campi Flegrei caldera unrest: Discriminating magma intrusions from hydrothermal effects and implications for possible evolution[J],2019,188.
APA	Troise C.,De Natale G.,Schiavone R.,Somma R.,&Moretti R..(2019).The Campi Flegrei caldera unrest: Discriminating magma intrusions from hydrothermal effects and implications for possible evolution.EARTH-SCIENCE REVIEWS,188.
MLA	Troise C.,et al."The Campi Flegrei caldera unrest: Discriminating magma intrusions from hydrothermal effects and implications for possible evolution".EARTH-SCIENCE REVIEWS 188(2019).