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EnglishIn order to investigate the variability of helium degassing in continental regions, its release from rocks and emission into the atmosphere, here we studied the degassing of volatiles in a seismically active region of northern Italy (MwMAX = 6) at the Nirano-Regnano mud volcanic system. The emitted gases in the study area are CH4–dominated and it is the carrier for helium (He) transfer through the crust. Carbon and He isotopes unequivocally indicate that crustal-derived fluids dominate these systems. An high-resolution 3-dimensional reconstruction of the gas reservoirs feeding the observed gas emissions at the surface permits to estimate the amount of He stored in the natural reservoirs. Our study demonstrated that the in-situ production of 4He in the crust and a long-lasting diffusion through the crust are not the main processes that rule the He degassing in the region. Furthermore, we demonstrated that micro-fracturation due to the field of stress that generates the local seismicity increases the release of He from the rocks and can sustain the excess of He in the natural reservoirs respect to the steady-state diffusive degassing. These results prove that (1) the transport of volatiles through the crust can be episodic as function of rock deformation and seismicity and (2) He can be used to highlight changes in the stress field and related earthquakes.
| Data di pubblicazione: | 2020 |
| Titolo: | Continental degassing of helium in an active tectonic setting (northern Italy): the role of seismicity |
| Autori: | |
| Citazione: | Buttitta D., Caracausi A., Chiaraluce L., Favara R., Gasparo Morticelli M., & Sulli A. (2020). Continental degassing of helium in an active tectonic setting (northern Italy): the role of seismicity. SCIENTIFIC REPORTS, 10(1), 1-13. |
| Rivista: | |
| Digital Object Identifier (DOI): | 10.1038/s41598-019-55678-7 |
| Abstract: | In order to investigate the variability of helium degassing in continental regions, its release from rocks and emission into the atmosphere, here we studied the degassing of volatiles in a seismically active region of northern Italy (MwMAX = 6) at the Nirano-Regnano mud volcanic system. The emitted gases in the study area are CH4–dominated and it is the carrier for helium (He) transfer through the crust. Carbon and He isotopes unequivocally indicate that crustal-derived fluids dominate these systems. An high-resolution 3-dimensional reconstruction of the gas reservoirs feeding the observed gas emissions at the surface permits to estimate the amount of He stored in the natural reservoirs. Our study demonstrated that the in-situ production of 4He in the crust and a long-lasting diffusion through the crust are not the main processes that rule the He degassing in the region. Furthermore, we demonstrated that micro-fracturation due to the field of stress that generates the local seismicity increases the release of He from the rocks and can sustain the excess of He in the natural reservoirs respect to the steady-state diffusive degassing. These results prove that (1) the transport of volatiles through the crust can be episodic as function of rock deformation and seismicity and (2) He can be used to highlight changes in the stress field and related earthquakes. |
| URL: | www.nature.com/srep/index.html |
| Settore Scientifico Disciplinare: | Settore GEO/02 - Geologia Stratigrafica E Sedimentologica Settore GEO/03 - Geologia Strutturale Settore GEO/08 - Geochimica E Vulcanologia |
| Appare nelle tipologie: | 1.01 Articolo in rivista |
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| buttitta et al 2020.pdf | Articolo principale | Versione Editoriale | Open Access Visualizza/Apri |
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