GSTDTAP  > 气候变化
DOI10.1002/2017GL076110
Pore Pressure Pulse Drove the 2012 Emilia (Italy) Series of Earthquakes
Pezzo, Giuseppe; De Gori, Pasquale; Lucente, Francesco Pio; Chiarabba, Claudio
2018-01-28
发表期刊GEOPHYSICAL RESEARCH LETTERS
ISSN0094-8276
EISSN1944-8007
出版年2018
卷号45期号:2页码:682-690
文章类型Article
语种英语
国家Italy
英文摘要

The 2012 Emilia earthquakes sequence is the first debated case in Italy of destructive event possibly induced by anthropic activity. During this sequence, two main earthquakes occurred separated by 9 days on contiguous thrust faults. Scientific commissions engaged by the Italian government reported complementary scenarios on the potential trigger mechanism ascribable to exploitation of a nearby oil field. In this study, we combine a refined geodetic source model constrained by precise aftershock locations and an improved tomographic model of the area to define the geometrical relation between the activated faults and investigate possible triggering mechanisms. An aftershock decay rate that deviates from the classical Omori-like pattern and Vp/Vs changes along the fault system suggests that natural pore pressure pulse drove the space-time evolution of seismicity and the activation of the second main shock.


Plain Language Summary Induced seismicity has increasingly become a major topic among Earth scientists. Concerns about a causative role played by the oil-gas extraction and/or the deep injection of disposable water in triggering earthquakes have grown fast in recent years, with many implications for public regulators and stakeholders. We present and discuss the 2012 Emilia (Italy) earthquakes sequence, which is the first debated case in Italy of destructive events possibly induced by anthropic activity. We use coseismic ground deformation measurements and seismic data to define the geometrical relation between the activated faults and investigate possible triggering mechanisms. Our results indicate that fluid pressure at the base of the system was responsible for triggering the two 2012 main earthquakes and exclude any anthropic trigger. Thus, cautious monitoring of seismicity, deformation, and pore pressure can recognize active processes along active faults that can potentially cause earthquakes. Such monitoring should be mandatory to conjugate exploitation activity in seismic active areas with safeness and sustainability.


领域气候变化
收录类别SCI-E
WOS记录号WOS:000425514300023
WOS关键词3-DIMENSIONAL CRUSTAL STRUCTURE ; ROMAGNA EARTHQUAKE ; SEISMIC SEQUENCE ; FLUID-FLOW ; AFTERSHOCKS ; CALIFORNIA ; INVERSION ; DEFORMATION ; APENNINES ; INSIGHTS
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
引用统计
文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/28649
专题气候变化
作者单位Ist Nazl Geofis & Vulcanol, Rome, Italy
推荐引用方式
GB/T 7714
Pezzo, Giuseppe,De Gori, Pasquale,Lucente, Francesco Pio,et al. Pore Pressure Pulse Drove the 2012 Emilia (Italy) Series of Earthquakes[J]. GEOPHYSICAL RESEARCH LETTERS,2018,45(2):682-690.
APA Pezzo, Giuseppe,De Gori, Pasquale,Lucente, Francesco Pio,&Chiarabba, Claudio.(2018).Pore Pressure Pulse Drove the 2012 Emilia (Italy) Series of Earthquakes.GEOPHYSICAL RESEARCH LETTERS,45(2),682-690.
MLA Pezzo, Giuseppe,et al."Pore Pressure Pulse Drove the 2012 Emilia (Italy) Series of Earthquakes".GEOPHYSICAL RESEARCH LETTERS 45.2(2018):682-690.
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