Matches in SemOpenAlex for { <https://semopenalex.org/work/W1970471607> ?p ?o ?g. }
- W1970471607 endingPage "54" @default.
- W1970471607 startingPage "30" @default.
- W1970471607 abstract "A compilation of the Marine Isotope Substage (MIS) 5.5 high stand (∼125 Ka) sites spanning the coastline of Italy allows a picture of the vertical displacement pattern affecting the Central Mediterranean coasts since the Late Pleistocene to be drawn. For each of the 246 listed sites, the accurate elevation of the high stand is defined through well-known markers. Coupled with a refined age assessment locally supported by new radiometric dating, these markers provide robust constraints on deformation. Significant alongshore differences in site elevation between +175 and −125 m a.s.l. resulted from the interplay of regional and local tectonic processes, including faulting and volcanic deformation. Whereas most of Sardinia's coasts and the northern Tyrrhenian Sea coasts are tectonically stable, the central Tyrrhenian Sea coasts display stable promontories, subsiding plains, and localized centres of weak uplift. Subsidence of the plains is related to extensional faulting locally enhanced by volcano-tectonic collapse, and weak uplift arising from magmatic processes. Rapid uplift of southern Calabria, northeast Sicily and the Jonian sea coasts probably reflects the extent of deep crustal delamination. The central Adriatic Sea shows weak thrust-related uplift, but foreland flexure in northern Adriatic and possibly southwestern Sicily results in locally intense regional subsidence. The rapidly uplifting regions are well correlated with the sectors of higher seismic release and surface horizontal motion documented by geodetic velocities. In this light, the MIS 5.5 marker indicates with a relatively high spatial resolution the vertical component of tectonic displacement and provides insight into the long-term tectonic processes of the Central Mediterranean orogen." @default.
- W1970471607 created "2016-06-24" @default.
- W1970471607 creator A5005305085 @default.
- W1970471607 creator A5005540912 @default.
- W1970471607 creator A5016724081 @default.
- W1970471607 creator A5017598913 @default.
- W1970471607 creator A5019470996 @default.
- W1970471607 creator A5025753900 @default.
- W1970471607 creator A5031759438 @default.
- W1970471607 creator A5037767942 @default.
- W1970471607 creator A5045405706 @default.
- W1970471607 creator A5046047833 @default.
- W1970471607 creator A5053488346 @default.
- W1970471607 creator A5058350352 @default.
- W1970471607 creator A5068127362 @default.
- W1970471607 creator A5061306074 @default.
- W1970471607 date "2006-03-01" @default.
- W1970471607 modified "2023-10-16" @default.
- W1970471607 title "Markers of the last interglacial sea-level high stand along the coast of Italy: Tectonic implications" @default.
- W1970471607 cites W1963864474 @default.
- W1970471607 cites W1964646401 @default.
- W1970471607 cites W1964810487 @default.
- W1970471607 cites W1967483268 @default.
- W1970471607 cites W1978167785 @default.
- W1970471607 cites W1979186423 @default.
- W1970471607 cites W1980146883 @default.
- W1970471607 cites W1988030596 @default.
- W1970471607 cites W1988743237 @default.
- W1970471607 cites W1991346788 @default.
- W1970471607 cites W1993402758 @default.
- W1970471607 cites W1997910557 @default.
- W1970471607 cites W2000695455 @default.
- W1970471607 cites W2002026394 @default.
- W1970471607 cites W2002630495 @default.
- W1970471607 cites W2003538528 @default.
- W1970471607 cites W2003858205 @default.
- W1970471607 cites W2003868383 @default.
- W1970471607 cites W2006832819 @default.
- W1970471607 cites W2009784602 @default.
- W1970471607 cites W2013573920 @default.
- W1970471607 cites W2014674516 @default.
- W1970471607 cites W2015055266 @default.
- W1970471607 cites W2015144933 @default.
- W1970471607 cites W2016827430 @default.
- W1970471607 cites W2020636511 @default.
- W1970471607 cites W2022839566 @default.
- W1970471607 cites W2025740359 @default.
- W1970471607 cites W2030609521 @default.
- W1970471607 cites W2030993933 @default.
- W1970471607 cites W2032891138 @default.
- W1970471607 cites W2033639081 @default.
- W1970471607 cites W2034626862 @default.
- W1970471607 cites W2037552928 @default.
- W1970471607 cites W2039563254 @default.
- W1970471607 cites W2040734165 @default.
- W1970471607 cites W2046888137 @default.
- W1970471607 cites W2049183734 @default.
- W1970471607 cites W2052847057 @default.
- W1970471607 cites W2052867711 @default.
- W1970471607 cites W2059070428 @default.
- W1970471607 cites W2059350495 @default.
- W1970471607 cites W2060125543 @default.
- W1970471607 cites W2063820228 @default.
- W1970471607 cites W2063858881 @default.
- W1970471607 cites W2064893459 @default.
- W1970471607 cites W2069165835 @default.
- W1970471607 cites W2070501546 @default.
- W1970471607 cites W2071910880 @default.
- W1970471607 cites W2072750627 @default.
- W1970471607 cites W2075263572 @default.
- W1970471607 cites W2078865347 @default.
- W1970471607 cites W2080068248 @default.
- W1970471607 cites W2080912283 @default.
- W1970471607 cites W2082150282 @default.
- W1970471607 cites W2082597970 @default.
- W1970471607 cites W2084669444 @default.
- W1970471607 cites W2085143818 @default.
- W1970471607 cites W2091137804 @default.
- W1970471607 cites W2099754161 @default.
- W1970471607 cites W2099826005 @default.
- W1970471607 cites W2104979774 @default.
- W1970471607 cites W2105352526 @default.
- W1970471607 cites W2109459276 @default.
- W1970471607 cites W2110629170 @default.
- W1970471607 cites W2112052262 @default.
- W1970471607 cites W2118821165 @default.
- W1970471607 cites W2121454423 @default.
- W1970471607 cites W2127213266 @default.
- W1970471607 cites W2127493276 @default.
- W1970471607 cites W2128586047 @default.
- W1970471607 cites W2132037307 @default.
- W1970471607 cites W2134818718 @default.
- W1970471607 cites W2141367321 @default.
- W1970471607 cites W2152666851 @default.
- W1970471607 cites W2163475804 @default.
- W1970471607 cites W2164873249 @default.
- W1970471607 cites W2165229426 @default.
- W1970471607 cites W2167970659 @default.