Matches in SemOpenAlex for { <https://semopenalex.org/work/W2765210206> ?p ?o ?g. }
- W2765210206 endingPage "4210" @default.
- W2765210206 startingPage "4186" @default.
- W2765210206 abstract "Abstract In the Ionian Sea, the subduction of the Nubia plate underneath the Eurasia plate leads to an important sediment remobilization on the Calabrian Arc and the Mediterranean Ridge. These events are often associated with earthquakes and tsunamis. In this study, we analyze gravity‐driven deposits in order to establish their recurrence time on the Calabrian Arc and the western Mediterranean Ridge. Four gravity cores collected on ridges and slope basins of accretionary prisms record turbidites, megaturbidites, slumping and micro‐faults over the last 330,000 years. These turbidites were dated by correlation with a hemipelagic core with a multi‐proxy approach: radiometric dating, δ18O, b* colour curve, sapropels and tephrochronology. The origin of the gravity‐driven deposits was studied with a sedimentary approach: grain‐size, lithology, thin section, geochemistry of volcanic glass. The results suggest three periods of presence/absence of gravity‐driven deposits: a first on the western lobe of the Calabrian Arc between 330,000 and 250,000 years, a second between 120,000 years and present day on the eastern lobe of the Calabrian Arc and over the last 60,000 years on the western lobe, and a third on the Mediterranean Ridge over the last 37,000 years. Return times for gravity‐driven deposits are around 1,000 years during the most important record periods. The turbidite activity also highlights the presence of volcaniclastic turbidites that seems to be link to the Etna changing morphology over the last 320,000 years." @default.
- W2765210206 created "2017-11-10" @default.
- W2765210206 creator A5009038171 @default.
- W2765210206 creator A5033811746 @default.
- W2765210206 creator A5057317475 @default.
- W2765210206 creator A5064124759 @default.
- W2765210206 creator A5082278304 @default.
- W2765210206 creator A5083213304 @default.
- W2765210206 creator A5085329585 @default.
- W2765210206 date "2017-11-01" @default.
- W2765210206 modified "2023-10-05" @default.
- W2765210206 title "Gravity‐Driven Deposits in an Active Margin (Ionian Sea) Over the Last 330,000 Years" @default.
- W2765210206 cites W1590864576 @default.
- W2765210206 cites W1596024932 @default.
- W2765210206 cites W1650803202 @default.
- W2765210206 cites W1657962187 @default.
- W2765210206 cites W1714529472 @default.
- W2765210206 cites W1774199323 @default.
- W2765210206 cites W1805930679 @default.
- W2765210206 cites W1949478573 @default.
- W2765210206 cites W1964410348 @default.
- W2765210206 cites W1967266368 @default.
- W2765210206 cites W1967733640 @default.
- W2765210206 cites W1968615177 @default.
- W2765210206 cites W1968726232 @default.
- W2765210206 cites W1970392311 @default.
- W2765210206 cites W1971369540 @default.
- W2765210206 cites W1972076708 @default.
- W2765210206 cites W1973580486 @default.
- W2765210206 cites W1974867019 @default.
- W2765210206 cites W1974905100 @default.
- W2765210206 cites W1976090220 @default.
- W2765210206 cites W1978055661 @default.
- W2765210206 cites W1980548523 @default.
- W2765210206 cites W1982112763 @default.
- W2765210206 cites W1986187203 @default.
- W2765210206 cites W1986913346 @default.
- W2765210206 cites W1988869537 @default.
- W2765210206 cites W1991667433 @default.
- W2765210206 cites W1993708701 @default.
- W2765210206 cites W1997578008 @default.
- W2765210206 cites W2007903703 @default.
- W2765210206 cites W2008048913 @default.
- W2765210206 cites W2010399187 @default.
- W2765210206 cites W2010932388 @default.
- W2765210206 cites W2015233904 @default.
- W2765210206 cites W2015515846 @default.
- W2765210206 cites W2017999067 @default.
- W2765210206 cites W2018516398 @default.
- W2765210206 cites W2020024379 @default.
- W2765210206 cites W2020715324 @default.
- W2765210206 cites W2023815011 @default.
- W2765210206 cites W2024111040 @default.
- W2765210206 cites W2027287476 @default.
- W2765210206 cites W2033639081 @default.
- W2765210206 cites W2038238045 @default.
- W2765210206 cites W2047781460 @default.
- W2765210206 cites W2048403692 @default.
- W2765210206 cites W2050262541 @default.
- W2765210206 cites W2057504811 @default.
- W2765210206 cites W2057996409 @default.
- W2765210206 cites W2059013307 @default.
- W2765210206 cites W2062490991 @default.
- W2765210206 cites W2065204617 @default.
- W2765210206 cites W2065348283 @default.
- W2765210206 cites W2072927700 @default.
- W2765210206 cites W2072981849 @default.
- W2765210206 cites W2075013000 @default.
- W2765210206 cites W2076203298 @default.
- W2765210206 cites W2076320763 @default.
- W2765210206 cites W2076919476 @default.
- W2765210206 cites W2077215331 @default.
- W2765210206 cites W2077267127 @default.
- W2765210206 cites W2077648240 @default.
- W2765210206 cites W2077667027 @default.
- W2765210206 cites W2078167754 @default.
- W2765210206 cites W2080313786 @default.
- W2765210206 cites W2080958987 @default.
- W2765210206 cites W2080969185 @default.
- W2765210206 cites W2088514454 @default.
- W2765210206 cites W2089028175 @default.
- W2765210206 cites W2089883709 @default.
- W2765210206 cites W2091206547 @default.
- W2765210206 cites W2093275789 @default.
- W2765210206 cites W2100981277 @default.
- W2765210206 cites W2101372386 @default.
- W2765210206 cites W2105166733 @default.
- W2765210206 cites W2113483124 @default.
- W2765210206 cites W2115563306 @default.
- W2765210206 cites W2122341820 @default.
- W2765210206 cites W2135955762 @default.
- W2765210206 cites W2136208295 @default.
- W2765210206 cites W2136633733 @default.
- W2765210206 cites W2139857660 @default.
- W2765210206 cites W2142450304 @default.
- W2765210206 cites W2145905489 @default.
- W2765210206 cites W2147762586 @default.
- W2765210206 cites W2150686037 @default.