FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2155117654> ?p ?o ?g. }

• W2155117654 endingPage "1094" @default.
• W2155117654 startingPage "1078" @default.
• W2155117654 abstract "To gain a better insight of the hydrogeology and the location of the main tectonic faults of Stromboli volcano in Italy, we collected electrical resistivity measurements, soil CO2 concentrations, temperature and self-potential measurements along two profiles. These two profiles started at the village of Ginostra in the southwest part of the island. The first profile (4.8 km in length) ended up at the village of Scari in the north east part of the volcano and the second one (3.5 km in length) at Forgia Vecchia beach, in the eastern part of the island. These data were used to provide insights regarding the position of shallow aquifers and the extension of the hydrothermal system. This large-scale study is complemented by two high-resolution studies, one at the Pizzo area (near the active vents) and one at Rina Grande where flank collapse areas can be observed. The Pizzo corresponds to one of the main degassing structure of the hydrothermal system. The main degassing area is localized along a higher permeability area corresponding to the head of the gliding plane of the Rina Grande sector collapse. We found that the self-potential data reveal the position of an aquifer above the villages of Scari and San Vincenzo. We provide an estimate of the depth of this aquifer from these data. The lateral extension of the hydrothermal system (resistivity ∼15–60 ohm m) is broader than anticipated extending in the direction of the villages of Scari and San Vincenzo (in agreement with temperature data recorded in shallow wells). The lateral extension of the hydrothermal system reaches the lower third of the Rina Grande sector collapse area in the eastern part of the island. The hydrothermal body in this area is blocked by an old collapse boundary. This position of the hydrothermal body is consistent with low values of the magnetization (<2.5 A m−1) from previously published work. The presence of the hydrothermal body below Rina Grande raises questions about the mechanical stability of this flank of the edifice." @default.
• W2155117654 created "2016-06-24" @default.
• W2155117654 creator A5008239839 @default.
• W2155117654 creator A5012032240 @default.
• W2155117654 creator A5018043429 @default.
• W2155117654 creator A5021932273 @default.
• W2155117654 creator A5027761636 @default.
• W2155117654 creator A5036960055 @default.
• W2155117654 creator A5039949232 @default.
• W2155117654 creator A5041229166 @default.
• W2155117654 creator A5044511715 @default.
• W2155117654 creator A5053299360 @default.
• W2155117654 creator A5060874148 @default.
• W2155117654 creator A5062286415 @default.
• W2155117654 creator A5070537087 @default.
• W2155117654 creator A5072791126 @default.
• W2155117654 creator A5089672144 @default.
• W2155117654 creator A5091215598 @default.
• W2155117654 date "2011-09-01" @default.
• W2155117654 modified "2023-10-06" @default.
• W2155117654 title "Hydrogeology of Stromboli volcano, Aeolian Islands (Italy) from the interpretation of resistivity tomograms, self-potential, soil temperature and soil CO2 concentration measurements" @default.
• W2155117654 cites W1498373505 @default.
• W2155117654 cites W1567708401 @default.
• W2155117654 cites W1931441157 @default.
• W2155117654 cites W1967037756 @default.
• W2155117654 cites W1968103857 @default.
• W2155117654 cites W1968676811 @default.
• W2155117654 cites W1968692372 @default.
• W2155117654 cites W1975469220 @default.
• W2155117654 cites W1976225490 @default.
• W2155117654 cites W1984540121 @default.
• W2155117654 cites W1986867161 @default.
• W2155117654 cites W1989137372 @default.
• W2155117654 cites W1993071847 @default.
• W2155117654 cites W2000295358 @default.
• W2155117654 cites W2002387161 @default.
• W2155117654 cites W2006243771 @default.
• W2155117654 cites W2006447461 @default.
• W2155117654 cites W2009584263 @default.
• W2155117654 cites W2011896880 @default.
• W2155117654 cites W2013123131 @default.
• W2155117654 cites W2027128207 @default.
• W2155117654 cites W2028042427 @default.
• W2155117654 cites W2030328808 @default.
• W2155117654 cites W2031401646 @default.
• W2155117654 cites W2033524684 @default.
• W2155117654 cites W2035364981 @default.
• W2155117654 cites W2038370704 @default.
• W2155117654 cites W2040741110 @default.
• W2155117654 cites W2042790773 @default.
• W2155117654 cites W2043916798 @default.
• W2155117654 cites W2045380392 @default.
• W2155117654 cites W2051792052 @default.
• W2155117654 cites W2052315633 @default.
• W2155117654 cites W2057613181 @default.
• W2155117654 cites W2060771035 @default.
• W2155117654 cites W2063190334 @default.
• W2155117654 cites W2063918130 @default.
• W2155117654 cites W2066501581 @default.
• W2155117654 cites W2072446965 @default.
• W2155117654 cites W2073471899 @default.
• W2155117654 cites W2076313097 @default.
• W2155117654 cites W2076526690 @default.
• W2155117654 cites W2077988768 @default.
• W2155117654 cites W2084451306 @default.
• W2155117654 cites W2085178881 @default.
• W2155117654 cites W2085807184 @default.
• W2155117654 cites W2088827609 @default.
• W2155117654 cites W2090555574 @default.
• W2155117654 cites W2099587512 @default.
• W2155117654 cites W2119003181 @default.
• W2155117654 cites W2127037336 @default.
• W2155117654 cites W2133513614 @default.
• W2155117654 cites W2142290446 @default.
• W2155117654 cites W2149889276 @default.
• W2155117654 cites W2153779120 @default.
• W2155117654 cites W2168358439 @default.
• W2155117654 cites W2169694900 @default.
• W2155117654 cites W2171234904 @default.
• W2155117654 doi "https://doi.org/10.1111/j.1365-246x.2011.05112.x" @default.
• W2155117654 hasPublicationYear "2011" @default.
• W2155117654 type Work @default.
• W2155117654 sameAs 2155117654 @default.
• W2155117654 citedByCount "71" @default.
• W2155117654 countsByYear W21551176542012 @default.
• W2155117654 countsByYear W21551176542013 @default.
• W2155117654 countsByYear W21551176542014 @default.
• W2155117654 countsByYear W21551176542015 @default.
• W2155117654 countsByYear W21551176542016 @default.
• W2155117654 countsByYear W21551176542017 @default.
• W2155117654 countsByYear W21551176542018 @default.
• W2155117654 countsByYear W21551176542019 @default.
• W2155117654 countsByYear W21551176542020 @default.
• W2155117654 countsByYear W21551176542021 @default.
• W2155117654 countsByYear W21551176542022 @default.
• W2155117654 countsByYear W21551176542023 @default.
• W2155117654 crossrefType "journal-article" @default.
• W2155117654 hasAuthorship W2155117654A5008239839 @default.

• next