2016
DOI: 10.1007/s10712-016-9380-4
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3D Subsoil Model of the San Biagio ‘Salinelle’ Mud Volcanoes (Belpasso, Sicily) derived from Geophysical Surveys

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Cited by 26 publications
(7 citation statements)
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“…This morphometric structure is typical of uplifting areas and therefore relative decrease in the base level. This suggests an inflection process of the volcano ground surface induced by an increase in fluid pressure inside of a shallower stagnation chamber which is located at a depth of about 30 m (Imposa et al, 2018). The stagnation chamber has a "sill-like" geometry, a radius of about 50 m and a thickness of about 30 m. This morphostructural configuration supported by geophysical data configures the active geological structure as a high potential geological hazard.…”
mentioning
confidence: 74%
“…This morphometric structure is typical of uplifting areas and therefore relative decrease in the base level. This suggests an inflection process of the volcano ground surface induced by an increase in fluid pressure inside of a shallower stagnation chamber which is located at a depth of about 30 m (Imposa et al, 2018). The stagnation chamber has a "sill-like" geometry, a radius of about 50 m and a thickness of about 30 m. This morphostructural configuration supported by geophysical data configures the active geological structure as a high potential geological hazard.…”
mentioning
confidence: 74%
“…Moreover, the morpho-structural study of mud volcanoes distributed along the frontal sector of the Sicilian collisional belt (San Biagio, Santa Barbara and Aragona villages) (Fig. 1) (Imposa et al, 2016;Madonia et al, 2011) also represents a clue that could be used as a proxy for supplementary stress and strain indicators. In fact, on a regional scale, mud volcanoes in active fold-and-thrust belts may occur over wider areas or may cluster along discrete structures, where the generation of overpressures is expected to establish a positive feedback loop allowing for fault movement and mud volcanism.…”
Section: Bibliografiamentioning
confidence: 99%
“…In recent years, many authors have also successfully tested the reliability of HVSRs in estimating local effects linked to the presence of different morphological conditions such as landslides, faults, etc. [15][16][17][18][19][20]. Moreover, being a non-invasive technique, it can be used in cultural heritage sites [21][22][23].…”
Section: Introductionmentioning
confidence: 99%