Articles | Volume 11, issue 2
Solid Earth, 11, 719–739, 2020
https://doi.org/10.5194/se-11-719-2020
Solid Earth, 11, 719–739, 2020
https://doi.org/10.5194/se-11-719-2020

Research article 30 Apr 2020

Research article | 30 Apr 2020

An active tectonic field for CO2 storage management: the Hontomín onshore case study (Spain)

Raúl Pérez-López et al.

Related subject area

Subject area: Tectonic plate interactions, magma genesis, and lithosphere deformation at all scales | Editorial team: Structural geology and tectonics, rock physics, experimental deformation | Discipline: Structural geology
Analysis of deformation bands associated with the Trachyte Mesa intrusion, Henry Mountains, Utah: implications for reservoir connectivity and fluid flow around sill intrusions
Penelope I. R. Wilson, Robert W. Wilson, David J. Sanderson, Ian Jarvis, and Kenneth J. W. McCaffrey
Solid Earth, 12, 95–117, https://doi.org/10.5194/se-12-95-2021,https://doi.org/10.5194/se-12-95-2021, 2021
Short summary
Characterization of discontinuities in potential reservoir rocks for geothermal applications in the Rhine-Ruhr metropolitan area (Germany)
Martin Balcewicz, Benedikt Ahrens, Kevin Lippert, and Erik H. Saenger
Solid Earth, 12, 35–58, https://doi.org/10.5194/se-12-35-2021,https://doi.org/10.5194/se-12-35-2021, 2021
Short summary
On a new robust workflow for the statistical and spatial analysis of fracture data collected with scanlines (or the importance of stationarity)
Andrea Bistacchi, Silvia Mittempergher, Mattia Martinelli, and Fabrizio Storti
Solid Earth, 11, 2535–2547, https://doi.org/10.5194/se-11-2535-2020,https://doi.org/10.5194/se-11-2535-2020, 2020
Short summary
Micro- and nano-porosity of the active Alpine Fault zone, New Zealand
Martina Kirilova, Virginia Toy, Katrina Sauer, François Renard, Klaus Gessner, Richard Wirth, Xianghui Xiao, and Risa Matsumura
Solid Earth, 11, 2425–2438, https://doi.org/10.5194/se-11-2425-2020,https://doi.org/10.5194/se-11-2425-2020, 2020
Short summary
Unraveling the origins and P-T-t evolution of the allochthonous Sobrado unit (Órdenes Complex, NW Spain) using combined U–Pb titanite, monazite and zircon geochronology and rare-earth element (REE) geochemistry
José Manuel Benítez-Pérez, Pedro Castiñeiras, Juan Gómez-Barreiro, José R. Martínez Catalán, Andrew Kylander-Clark, and Robert Holdsworth
Solid Earth, 11, 2303–2325, https://doi.org/10.5194/se-11-2303-2020,https://doi.org/10.5194/se-11-2303-2020, 2020
Short summary

Cited articles

Alcalde, J., Martí, D., Calahorrano, A., Marzan, I., Ayarza, P., Carbonell, R., Juhlin, C., and Pérez-Estaún, A.: Active seismic characterization experiments of the Hontomín research facility for geological storage of CO2, Spain, Int. J. Greenh. Gas Con., 19, 785–795, https://doi.org/10.1016/j.ijggc.2013.01.039, 2013. 
Alcalde, J., Marzán, I., Saura, E., Martí, D., Ayarza, P., Juhlin, C., Pérez-Estaún, A., and Carbonell, R.: 3D geological characterization of the Hontomín CO2 storage site, Spain: Multidisciplinary approach from seismic, well-log and regional data, Tectonophysics, 627, 6–25, https://doi.org/10.1016/j.tecto.2014.04.025, 2014. 
Allmendinger, R. W., Cardozo, N. C., and Fisher, D.: Structural Geology Algorithms: Vectors & Tensors, Cambridge University Press, Cambridge, England, 289 pp., 2012. 
Álvarez-Gómez, J. A.: FMC: a one-liner python program to manage, classify and plot focal mechanisms, in: EGU General Assembly, 27 April–2 May 2014, Vienna, Austria, EGU2014-10887, 2014. 
Anderson, E. M.: The Dynamics of Faulting and Dyke Formation with application to Britain, 2nd Edn., Oliver and Boyd, Edinburgh, 206 pp., 1951. 
Download
Short summary
Long-term monitoring of CO2 of onshore storage has to consider thousands of years as a medium lifetime of the storage. In this wide time interval, the stress and strain properties of the reservoir change and earthquakes could occur. Therefore, we have to identify those fault sets which can be reactivated by changing the stress conditions. We need to know the role of active fault sets and model the changing conditions to prevent induced seismicity.