http://www.cnr.it/ontology/cnr/individuo/prodotto/ID286456
Fluid injection induced seismicity reveals a NE dipping fault in the southeastern sector of the High Agri Valley (southern Italy) (Articolo in rivista)
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- Fluid injection induced seismicity reveals a NE dipping fault in the southeastern sector of the High Agri Valley (southern Italy) (Articolo in rivista) (literal)
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- 2014-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1002/2014GL060948 (literal)
- Alternative label
Stabile, T.A. a , Giocoli, A. ab, Perrone, A. a, Piscitelli, S. a, Lapenna, V. a (2014)
Fluid injection induced seismicity reveals a NE dipping fault in the southeastern sector of the High Agri Valley (southern Italy)
in Geophysical research letters; American Geophysical Union, Washington (Stati Uniti d'America)
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- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Stabile, T.A. a , Giocoli, A. ab, Perrone, A. a, Piscitelli, S. a, Lapenna, V. a (literal)
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- http://onlinelibrary.wiley.com/doi/10.1002/2014GL060948/abstract (literal)
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- a. Consiglio Nazionale delle Ricerche, Istituto di Metodologie per l'Analisi Ambientale 85050 Tito Scalo (PZ) Italy
b. Now at Agenzia nazionale per le nuove tecnologie, l'energia e lo sviluppo economico sostenibile Rome Italy (literal)
- Titolo
- Fluid injection induced seismicity reveals a NE dipping fault in the southeastern sector of the High Agri Valley (southern Italy) (literal)
- Abstract
- On 2 June 2006 the wastewater produced during the oil and gas field exploitation in High Agri Valley (southern Italy) started to be managed by disposal through pumping the fluids back into the subsurface at the Costa Molina 2 (CM2) injection well, located in the southeastern sector of the valley. The onset of microearthquakes (Ml2) after 4days at about 1.3km SW of CM2 well suggests fluid injection induced seismicity by the diffusion of pore pressure. Moreover, the space-time evolution of 196 high-resolution relocated events reveals a previously unmapped NE dipping fault. We investigate the physical processes related to the fluid injection induced seismicity and delineate the previously unmapped fault by jointly analyzing seismicity data, geological observations, fluid injection data, the stratigraphic log of the CM2 well, and the electrical resistivity tomography survey carried out in the study area. (literal)
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