2022
DOI: 10.1016/j.enggeo.2022.106741
|View full text |Cite
|
Sign up to set email alerts
|

A geology-based 3D velocity model of the Amatrice Basin (Central Italy)

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
2

Citation Types

0
2
0

Year Published

2023
2023
2024
2024

Publication Types

Select...
2
1

Relationship

1
2

Authors

Journals

citations
Cited by 3 publications
(4 citation statements)
references
References 59 publications
0
2
0
Order By: Relevance
“…As an example, once populated with the values of seismic velocity, the 3D geological model can find several applications in seismological studies. It can be used to improve the procedure and reduce the uncertainties during earthquake location, contribute to the calculation of more accurate focal mechanisms and perform wavepropagation and ground-motion simulations (e.g., Magistrale et al, 1996;Süss et al, 2001;Molinari et al, 2015;Livani et al, 2022). The 3D model also represents a starting model in perturbation studies, such as linearized inversions of travel times for crustal velocities (e.g., Magistrale and Day, 1999) or for studies related to the seismic waveforms for crustal structure and, moreover, it can be used to derive densities and compare them to gravity observations (Roy and Clayton, 1999).…”
Section: Discussionmentioning
confidence: 99%
See 1 more Smart Citation
“…As an example, once populated with the values of seismic velocity, the 3D geological model can find several applications in seismological studies. It can be used to improve the procedure and reduce the uncertainties during earthquake location, contribute to the calculation of more accurate focal mechanisms and perform wavepropagation and ground-motion simulations (e.g., Magistrale et al, 1996;Süss et al, 2001;Molinari et al, 2015;Livani et al, 2022). The 3D model also represents a starting model in perturbation studies, such as linearized inversions of travel times for crustal velocities (e.g., Magistrale and Day, 1999) or for studies related to the seismic waveforms for crustal structure and, moreover, it can be used to derive densities and compare them to gravity observations (Roy and Clayton, 1999).…”
Section: Discussionmentioning
confidence: 99%
“…To this end, the definition of the physical and geometrical attributes of the outcropping and subsurface geological units provides fundamental knowledge for several scientific topics and many engineering plans and operations. As an example, the integration of physical parameters of subsurface geological units into a well-defined 3D model can be applied to (i) to reduce the uncertainties for earthquake location, contributing to the calculation of more accurate focal mechanisms and performing wavepropagation and ground-motion simulations (e.g., Magistrale et al, 1996;Süss et al, 2001;Molinari et al, 2015;Livani et al, 2022), and (ii) understand, simulate, and predict the response of the geological body to subsurface natural and anthropic processes. The latter is the case of 3D geomechanical numerical models, which represent effective tools to evaluate and predict the possible effects -both at the surface and in the subsurface -of geofluid extraction and storage, to guarantee a safe management of such activities as well as to quantify and better understand the ongoing geological processes (e.g., tectonic deformation, natural subsidence, etc.…”
Section: Introductionmentioning
confidence: 99%
“…It can be used to improve the procedure and to reduce the uncertainties during earthquake location, it can contribute to the calculation of more accurate focal mechanisms, and it can perform wave propagation and ground motion sim-ulations (e.g. Magistrale et al, 1999;Süss et al, 2001;Molinari et al, 2015;Livani et al, 2022). The 3D model also represents a starting model in perturbation studies, such as linearized inversions of travel times for crustal velocities (e.g.…”
Section: Discussionmentioning
confidence: 99%
“…As an example, the integration of physical parameters of subsurface geological units into a well-defined 3D model can be applied to (i) reduce the uncertainties for earthquake location, contributing to the calculation of more accurate focal mechanisms and performing wave propagation and ground motion simulations (e.g. Magistrale et al, 1996;Süss et al, 2001;Molinari et al, 2015;Livani et al, 2022); and (ii) understand, simulate, and predict the response of the geological body to subsurface natural and anthropic processes. The latter is the case for 3D geomechanical numerical models, which represent effective tools for the evaluation and prediction of the possible effects -both at the surface and in the subsurface -of geofluid extraction and storage to guarantee the safe management of such activities, as well as to quan-tify and better understand the ongoing geological processes (e.g.…”
Section: Introductionmentioning
confidence: 99%