Anthropogenic seismicity in Italy and its relation to tectonics: State of the art and perspectives. (March 2018)

• Record Type: Journal Article
• Authors: Braun, Thomas; Cesca, Simone; Kühn, Daniela; Martirosian-Janssen, Araksi; Dahm, Torsten
• Is Part Of: Anthropocene. Volume 21(2018)
• Page Start: 80
• Page End: 94
• Publication Date: 2018-03
• Subjects: 00-01 -- 99-00; Triggered/induced seismicity -- Italy -- Carbon dioxide extraction -- Geothermal exploitation -- Reservoir impoundment -- Mt. Amiata -- Upper Tiber Valley; Nature -- Effect of human beings on -- Periodicals; Human ecology -- Periodicals; 304.2
• DOI: 10.1016/j.ancene.2018.02.001
• Languages: English
• ISSNs: 2213-3054

Abstract

Abstract: Since hydrofracking is used for shale gas production, human caused seismicity has become a subject of increasing interest. Seismic monitoring is common for earthquakes generated by human operations like mining, reservoir impoundments, hydrocarbon and geothermal production, as well as reinjection of fluids. In Italy the M w 6.1 Reggio-Emilia earthquake of 20 th May 2012 triggered particular interest in anthropogenic seismicity. It also raised the question of whether hydrocarbon exploitation induced variations in crustal stress that influenced the generation of these earthquakes. The Italian government commissioned a technical report compiling cases of documented and hypothesized anthropogenic seismicity. This paper reviews these cases, on the basis of previously published works, and additional new analyses. Three cases of seismicity in Central Italy, occurring close to anthropogenic activities, are: (i) extraction of carbon dioxide (CO2 ) from a borehole near Pieve Santo Stefano, (ii) the impoundment of the Montedoglio reservoir and (iii) geothermal energy production at Mt. Amiata. Since the sites are situated in the seismically active area of the Northern Apennines, we illustrate both by standard seismological analysis as well as by modeling to tackle the challenge of discriminating anthropogenic from natural seismicity.