2012
DOI: 10.1007/s10967-012-2310-0
|View full text |Cite
|
Sign up to set email alerts
|

An analytical algorithm for designing radon monitoring network to predict the location and magnitude of earthquakes

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
5

Citation Types

0
6
0
1

Year Published

2013
2013
2020
2020

Publication Types

Select...
10

Relationship

1
9

Authors

Journals

citations
Cited by 18 publications
(7 citation statements)
references
References 27 publications
0
6
0
1
Order By: Relevance
“…Surveys of soil gas have been commonly used to trace buried faults and to study the behavior of endogenous gases of specific origins in the shallow environment (i.e., trace gases such as radon and helium, and carrier gases such as carbon dioxide, nitrogen, methane, etc.) [1][2][3][4][5][6][7][8] and have received significant attention over the last few years as earthquake precursors [6,[9][10][11][12][13][14][15]. In addition, changes in stress/strain associated with seismic activity may force the migration of crustal fluid, in particular along active faults, thereby altering the geochemical characteristics of the surface fault zone [16][17][18].…”
Section: Introductionmentioning
confidence: 99%
“…Surveys of soil gas have been commonly used to trace buried faults and to study the behavior of endogenous gases of specific origins in the shallow environment (i.e., trace gases such as radon and helium, and carrier gases such as carbon dioxide, nitrogen, methane, etc.) [1][2][3][4][5][6][7][8] and have received significant attention over the last few years as earthquake precursors [6,[9][10][11][12][13][14][15]. In addition, changes in stress/strain associated with seismic activity may force the migration of crustal fluid, in particular along active faults, thereby altering the geochemical characteristics of the surface fault zone [16][17][18].…”
Section: Introductionmentioning
confidence: 99%
“…and [e.g., King, 1985;Baubron et al, 2002;Ciotoli et al, 2007;Fu et al, 2008;Walia et al, S 2009;Ciotoli et al, 2014;Bigi et al, 2014;Sciarra et al, 2014]. Furthermore, over the past several years' soil gases has captured considerable attention as earthquake precursors [Wakita et al, 1980;Reddy et al, 2004;Walia et al, 2009;Perez et al, 2007;Ghosh et al, 2009;Hashemi et al, 2013;Petraki et al, 2015], in fact that the stress/strain changes related to seismic activity may force crustal fluid to migrate up, especially along active faults, thereby altering the geochemical characteristics of the fault zone at surface [Rice, 1992;Sibson, 2000;Collettini et al, 2008]. The migration of these gases by diffusion and/or advection along buried active faults can generate shallow anomalies with concentrations significantly higher than background levels; these anomalies can provide reliable information about the location and the geometry of the shallow fracturing zone, as well as about the permeability within the fault zone [King et al, 1996;Baubron et al, 2002;Ciotoli et al, 2007;Annunziatellis et al, 2008;Bigi et al, 2014;Sciarra et al, 2014].…”
Section: Introductionmentioning
confidence: 99%
“…In Kumar et al (2009), the radon anomalies observed in the region are connected with the seismic events of the Kangra Valley of north-west Himalayas. Hashemi et al (2013), Kloeden and Platen (2011) consider a new analytical algorithm to estimate location and magnitude of coming earthquakes by means of variations in radon concentration. The authors, using the radon monitoring for Kernal province, show that the optimum locations and magnitudes of earthquakes can be obtained within an acceptable range.…”
Section: Introductionmentioning
confidence: 99%