2015
DOI: 10.1007/s11069-015-1774-y
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Hazard assessment at the Quaternary La Garrotxa Volcanic Field (NE Iberia)

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Cited by 17 publications
(19 citation statements)
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“…Kernel density estimation (KDE), a nonparametric statistical method for estimating spatial density, is widely used by researchers as a method for predicting probable locations of future eruptive vents based solely on the observed locations of vents formed in the past (e.g., Richardson et al, 2012;Germa et al, 2013;El Difrawy et al, 2013;Bevilacqua et al, 2015;Bartolini et al, 2015;Galindo et al, 2016;Mazzarini et al, 2016;Tadini et al, 2017;van den Hove et al, 2017). In application of KDE, it is assumed that the past pattern of vent formation is governed by the same tectonic and magmatic factors that govern future vent formation.…”
Section: Introductionmentioning
confidence: 99%
“…Kernel density estimation (KDE), a nonparametric statistical method for estimating spatial density, is widely used by researchers as a method for predicting probable locations of future eruptive vents based solely on the observed locations of vents formed in the past (e.g., Richardson et al, 2012;Germa et al, 2013;El Difrawy et al, 2013;Bevilacqua et al, 2015;Bartolini et al, 2015;Galindo et al, 2016;Mazzarini et al, 2016;Tadini et al, 2017;van den Hove et al, 2017). In application of KDE, it is assumed that the past pattern of vent formation is governed by the same tectonic and magmatic factors that govern future vent formation.…”
Section: Introductionmentioning
confidence: 99%
“…For volcanic fields with low recurrence rates (e.g., Auckland Volcanic Field,~10 − 4 events/year; Bebbington and Cronin 2011), or scarce temporal data (e.g., Harrat Al-Madinah; El Difrawy et al 2013), it is usually assumed that the temporal component of the hazard assessment is independent of the spatial component (Bebbington 2013(Bebbington , 2015. Following this assumption, a long-term average recurrence rate (a stationary model) can be calculated for the whole field based on the number of events over a specific time interval, which has been a common approach for several volcanic fields (e.g., El Difrawy et al 2013;Runge et al 2014;Bartolini et al 2015;Gallant et al 2018;Nieto-Torres and Martin Del Pozzo 2019).…”
Section: Spatial Temporal and Volcanic Hazard Assessmentsmentioning
confidence: 99%
“…Several techniques to integrate multiple background data have been developed during the last few years (e.g., Cappello et al, 2012Cappello et al, , 2013Alcorn et al 2013;Becerril et al 2013Becerril et al , 2014Becerril et al , 2017El Difrawy et al 2013;Bartolini et al , 2015Gallant et al 2018;Jiménez et al 2018). Most of these approaches apply a similar statistical treatment of the available volcano-structural information resulting in spatial density maps showing the probability of vent location.…”
Section: Spatial Temporal and Volcanic Hazard Assessmentsmentioning
confidence: 99%
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