FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2045037953> ?p ?o ?g. }

• W2045037953 endingPage "173" @default.
• W2045037953 startingPage "155" @default.
• W2045037953 abstract "In this paper we give an overview of the recent geophysical, geochemical and volcanological studies concerning the island of Ischia within the geological and tectonic framework of Southern Italy. Ischia is an active volcanic field that had a complex volcanic history resulting from dominant explosive and minor effusive activity, several caldera collapses, and renewed volcanism from vents located inside the collapsed area. The island is morphologically dominated by Mt. Epomeo, the result of a prominent resurgence phenomenon taking place since ca. 33 ka BP, and responsible for ca. 900 m of total uplift, one of the largest known compared to the relatively small size of the caldera. The uplift was accompanied by activation of faults, seismic activity and renewal of volcanism, and may be considered a main factor for inducing slope instability. For Ischia, volcanological, petrological and geophysical studies are, at present, limited compared to the other active volcanoes of the Neapolitan Area. Furthermore, the island is characterized by high volcanic, seismic and hydrogeological risks. Thus, this review is aimed at highlighting aspects of the knowledge on Ischia that need more investigations, in order to better assess some characteristics of its structural setting. Features such as the precise location of the caldera boundaries and the depth of the magma chamber representing the drive for the resurgence still need to be well defined. A critical analysis of all lines of evidence relevant to the current theories about the island resurgence (resurgent block vs. resurgent dome) has been carried out. Our analysis reveals that the resurgent block model, differently from the resurgent dome model, is consistent with the most significant features, such as tilting of the resurgent block, faults type, dip and distribution at the edges of the block, and occurrence of most of the past 10 ka eruption vents on the eastern sector of the island. However, as both model require an input of fresh magma into the shallow plumbing system, it is not clear at present how much magma was necessary to achieve the measured uplift, and whether the drive was provided by magma or magmatic volatiles." @default.
• W2045037953 created "2016-06-24" @default.
• W2045037953 creator A5018329294 @default.
• W2045037953 creator A5028532880 @default.
• W2045037953 creator A5079984309 @default.
• W2045037953 date "2013-01-01" @default.
• W2045037953 modified "2023-10-10" @default.
• W2045037953 title "The structural setting of the Ischia Island (Phlegrean Volcanic District, Southern Italy): Inferences from geophysics and geochemistry" @default.
• W2045037953 cites W1541711731 @default.
• W2045037953 cites W1570418624 @default.
• W2045037953 cites W1743001425 @default.
• W2045037953 cites W1796730777 @default.
• W2045037953 cites W1925688530 @default.
• W2045037953 cites W1966329350 @default.
• W2045037953 cites W1967666903 @default.
• W2045037953 cites W1969205623 @default.
• W2045037953 cites W1975070272 @default.
• W2045037953 cites W1978696207 @default.
• W2045037953 cites W1979107676 @default.
• W2045037953 cites W1980251125 @default.
• W2045037953 cites W1985108036 @default.
• W2045037953 cites W1987545210 @default.
• W2045037953 cites W1988299808 @default.
• W2045037953 cites W1990662143 @default.
• W2045037953 cites W1993081536 @default.
• W2045037953 cites W1993608143 @default.
• W2045037953 cites W1993938132 @default.
• W2045037953 cites W1994972214 @default.
• W2045037953 cites W1995342172 @default.
• W2045037953 cites W1999757037 @default.
• W2045037953 cites W2003098478 @default.
• W2045037953 cites W2003247029 @default.
• W2045037953 cites W2005563146 @default.
• W2045037953 cites W2005856528 @default.
• W2045037953 cites W2009350839 @default.
• W2045037953 cites W2021255039 @default.
• W2045037953 cites W2023862052 @default.
• W2045037953 cites W2025084293 @default.
• W2045037953 cites W2027362689 @default.
• W2045037953 cites W2028669443 @default.
• W2045037953 cites W2033535870 @default.
• W2045037953 cites W2036789715 @default.
• W2045037953 cites W2039869957 @default.
• W2045037953 cites W2040636759 @default.
• W2045037953 cites W2049317419 @default.
• W2045037953 cites W2050089688 @default.
• W2045037953 cites W2050341136 @default.
• W2045037953 cites W2052460720 @default.
• W2045037953 cites W2054479665 @default.
• W2045037953 cites W2056612003 @default.
• W2045037953 cites W2057233333 @default.
• W2045037953 cites W2057996409 @default.
• W2045037953 cites W2067751327 @default.
• W2045037953 cites W2067759112 @default.
• W2045037953 cites W2070390543 @default.
• W2045037953 cites W2071133346 @default.
• W2045037953 cites W2072508332 @default.
• W2045037953 cites W2075395258 @default.
• W2045037953 cites W2082720521 @default.
• W2045037953 cites W2083565466 @default.
• W2045037953 cites W2083957989 @default.
• W2045037953 cites W2087903403 @default.
• W2045037953 cites W2089516766 @default.
• W2045037953 cites W2090312790 @default.
• W2045037953 cites W2094294558 @default.
• W2045037953 cites W2104144529 @default.
• W2045037953 cites W2108450218 @default.
• W2045037953 cites W2109291306 @default.
• W2045037953 cites W2117197878 @default.
• W2045037953 cites W2122370404 @default.
• W2045037953 cites W2122437766 @default.
• W2045037953 cites W2130425660 @default.
• W2045037953 cites W2131506862 @default.
• W2045037953 cites W2137532673 @default.
• W2045037953 cites W2142468129 @default.
• W2045037953 cites W2151808629 @default.
• W2045037953 cites W2153919782 @default.
• W2045037953 cites W2166656818 @default.
• W2045037953 cites W2282906445 @default.
• W2045037953 cites W2324301853 @default.
• W2045037953 cites W2887628283 @default.
• W2045037953 cites W2973891966 @default.
• W2045037953 cites W4234066087 @default.
• W2045037953 doi "https://doi.org/10.1016/j.jvolgeores.2012.10.002" @default.
• W2045037953 hasPublicationYear "2013" @default.
• W2045037953 type Work @default.
• W2045037953 sameAs 2045037953 @default.
• W2045037953 citedByCount "35" @default.
• W2045037953 countsByYear W20450379532013 @default.
• W2045037953 countsByYear W20450379532014 @default.
• W2045037953 countsByYear W20450379532015 @default.
• W2045037953 countsByYear W20450379532016 @default.
• W2045037953 countsByYear W20450379532017 @default.
• W2045037953 countsByYear W20450379532018 @default.
• W2045037953 countsByYear W20450379532019 @default.
• W2045037953 countsByYear W20450379532020 @default.
• W2045037953 countsByYear W20450379532021 @default.
• W2045037953 countsByYear W20450379532022 @default.

• next