globalchange  > 气候减缓与适应
DOI: 10.1002/2014GL059539
论文题名:
Clues to the cause of the 2011-2013 Campi Flegrei caldera unrest, Italy, from continuous GPS data
作者: Amoruso A.; Crescentini L.; Sabbetta I.; Demartino P.; Obrizzo F.; Tammaro U.
刊名: Geophysical Research Letters
ISSN: 0094-10084
EISSN: 1944-9815
出版年: 2014
卷: 41, 期:9
起始页码: 3081
结束页码: 3088
语种: 英语
英文关键词: caldera unrest ; Campi Flegrei ; deformation
Scopus关键词: Models ; Pressurization ; Caldera unrest ; Campi Flegrei ; Conceptual model ; Deep sources ; Magmatic fluids ; Near-real time ; Reference modeling ; Volcanic environment ; Deformation ; deformation ; GPS ; hydrothermal activity ; magmatism ; numerical model ; satellite data ; Campania [Italy] ; Campi Flegrei ; Italy ; Napoli [Campania]
英文摘要: From 2006 to spring 2013, Campi Flegrei (CF) caldera, Italy, was mostly uplifting at an increasing rate, particularly high from 2011. We show that the 2011-2013 accelerated uplift and 1980-2010 inflation and deflation phases can be explained by a two-source conceptual model similar to that proposed by Amoruso et al. (2014) (reference model). However, pressurization of the sole thin quasi-horizontal ∼4000m deep source, responsible for large-scale 1980-2010 deformation, can explain the whole 2011-2013 deformation, while activity of the shallower Solfatara hydrothermal source, responsible for residual 1980-2010 deformation, appears constant. These results suggest a predominantly magmatic unrest in 2011-2013. Near-real-time comparison of observations and reference model predictions can provide additional information for short-term eruption forecasting at CF; a similar approach could be followed also in other volcanic environments. Key Points The two sources of 1980-2010 CF deformation satisfy also the 2011-2013 unrest Pressurization of the sole ∼4000m deep source satisfies the whole deformation Injection of magma or magmatic fluids had a predominant role in the unrest © 2014. American Geophysical Union. All Rights Reserved.
URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84901923306&doi=10.1002%2f2014GL059539&partnerID=40&md5=92b3fcfac29511a248368ec75311cb68
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/7348
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作者单位: Department of Physics, University of Salerno, Fisciano, Italy

Recommended Citation:
Amoruso A.,Crescentini L.,Sabbetta I.,et al. Clues to the cause of the 2011-2013 Campi Flegrei caldera unrest, Italy, from continuous GPS data[J]. Geophysical Research Letters,2014-01-01,41(9).
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