FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4311479062> ?p ?o ?g. }

• W4311479062 endingPage "931" @default.
• W4311479062 startingPage "898" @default.
• W4311479062 abstract "Abstract Models of the formation of rifted margins have significantly evolved over the last decades by identifying new styles of crustal thinning and magmatic production. However, the expression of these different processes in the depositional environments of the overlying basins remains to be determined. Using only published data, we integrated the sedimentary evolution of 21 basins of the Equatorial, Central and South segments of the South Atlantic that record various styles of crustal thinning and magmatic production. To compare these basins that underwent rifting at different times, we developed a new type of analysis allowing to evaluate statistically the (dis)similarities in depositional environment trends by normalizing them to the tectonic phases of the basin (syn‐rift, transition and post‐rift) rather than the stratigraphic or absolute ages: The GeoDyNamical Analysis. We show that the timing of the long‐term retrograding mega‐sequence driven by lithosphere thinning depends on the deformation style and magma production. Along oblique margins of the Equatorial Segment, deepening initiated during syn‐rift because their narrow crustal thinning style favours rapid tectonic subsidence surpassing sediment supply. Along wide margins of the Central Segment, deepening is initiated later, at the end of the transition phase, because depth‐dependent thinning favours slow tectonic subsidence and late break‐up. Along magma‐rich margins of the South Segment, deepening is initiated during the transition phase, after volcanics stopped filling accommodation created by subsidence. In the Central Segment, evaporites accumulated during the second half of the transition phase, when crustal thinning ceased in the proximal margin and migrated to its distal part. Immediately before and during evaporites accumulation, sediments recorded continental and coastal depositional environments resulting from the limited thermal subsidence in the proximal margin domain. Evaporite deposition lasted until the initiation of retrograding mega‐sequence, at the onset of the post‐rift phase and the end of crustal thinning in the distal margin." @default.
• W4311479062 created "2022-12-26" @default.
• W4311479062 creator A5004052785 @default.
• W4311479062 creator A5009390490 @default.
• W4311479062 creator A5057673773 @default.
• W4311479062 creator A5062076169 @default.
• W4311479062 date "2022-12-21" @default.
• W4311479062 modified "2023-10-01" @default.
• W4311479062 title "Meta‐analysis of the long‐term stratigraphic evolution of rifted margin basins: The GeoDyNamical Analysis approach applied to the South Atlantic Ocean" @default.
• W4311479062 cites W1024272585 @default.
• W4311479062 cites W123756470 @default.
• W4311479062 cites W1532163399 @default.
• W4311479062 cites W1532165816 @default.
• W4311479062 cites W1548767494 @default.
• W4311479062 cites W1717248073 @default.
• W4311479062 cites W1748545007 @default.
• W4311479062 cites W1904788118 @default.
• W4311479062 cites W192834868 @default.
• W4311479062 cites W1966019257 @default.
• W4311479062 cites W1968904172 @default.
• W4311479062 cites W1970471156 @default.
• W4311479062 cites W1972123518 @default.
• W4311479062 cites W1983086091 @default.
• W4311479062 cites W1983467568 @default.
• W4311479062 cites W1986834399 @default.
• W4311479062 cites W1988166818 @default.
• W4311479062 cites W1989373633 @default.
• W4311479062 cites W1990185741 @default.
• W4311479062 cites W1999424907 @default.
• W4311479062 cites W1999779922 @default.
• W4311479062 cites W2001704267 @default.
• W4311479062 cites W2003041662 @default.
• W4311479062 cites W2004089187 @default.
• W4311479062 cites W2006032174 @default.
• W4311479062 cites W2008061945 @default.
• W4311479062 cites W2008461620 @default.
• W4311479062 cites W2009301865 @default.
• W4311479062 cites W2010899942 @default.
• W4311479062 cites W2014552552 @default.
• W4311479062 cites W2016521458 @default.
• W4311479062 cites W2017034624 @default.
• W4311479062 cites W2019534969 @default.
• W4311479062 cites W2021385170 @default.
• W4311479062 cites W2022660191 @default.
• W4311479062 cites W2023502216 @default.
• W4311479062 cites W2024361351 @default.
• W4311479062 cites W202682885 @default.
• W4311479062 cites W2030642602 @default.
• W4311479062 cites W2033818856 @default.
• W4311479062 cites W2033822779 @default.
• W4311479062 cites W2034013829 @default.
• W4311479062 cites W2035862022 @default.
• W4311479062 cites W2036235617 @default.
• W4311479062 cites W2036536910 @default.
• W4311479062 cites W2036853755 @default.
• W4311479062 cites W2038185107 @default.
• W4311479062 cites W2038991923 @default.
• W4311479062 cites W2039671643 @default.
• W4311479062 cites W2044732818 @default.
• W4311479062 cites W2046640225 @default.
• W4311479062 cites W2048496579 @default.
• W4311479062 cites W2048722474 @default.
• W4311479062 cites W2052639207 @default.
• W4311479062 cites W2054500555 @default.
• W4311479062 cites W2056353799 @default.
• W4311479062 cites W2058494246 @default.
• W4311479062 cites W2062921341 @default.
• W4311479062 cites W2065375137 @default.
• W4311479062 cites W2067237660 @default.
• W4311479062 cites W2068734771 @default.
• W4311479062 cites W2069299766 @default.
• W4311479062 cites W2070357922 @default.
• W4311479062 cites W2070651729 @default.
• W4311479062 cites W2073132195 @default.
• W4311479062 cites W2076258856 @default.
• W4311479062 cites W2076401680 @default.
• W4311479062 cites W2079851790 @default.
• W4311479062 cites W2080828102 @default.
• W4311479062 cites W2083690047 @default.
• W4311479062 cites W2087730351 @default.
• W4311479062 cites W2088978546 @default.
• W4311479062 cites W2090644297 @default.
• W4311479062 cites W2090673292 @default.
• W4311479062 cites W2092167782 @default.
• W4311479062 cites W2095411736 @default.
• W4311479062 cites W2096435869 @default.
• W4311479062 cites W2097971927 @default.
• W4311479062 cites W2100771039 @default.
• W4311479062 cites W2102364381 @default.
• W4311479062 cites W2105628276 @default.
• W4311479062 cites W2106862231 @default.
• W4311479062 cites W2108250538 @default.
• W4311479062 cites W2110585121 @default.
• W4311479062 cites W2116162173 @default.
• W4311479062 cites W2119313675 @default.
• W4311479062 cites W2124131175 @default.
• W4311479062 cites W2130495207 @default.
• W4311479062 cites W2131839205 @default.

• next