Matches in SemOpenAlex for { <https://semopenalex.org/work/W2890086380> ?p ?o ?g. }
- W2890086380 endingPage "132" @default.
- W2890086380 startingPage "115" @default.
- W2890086380 abstract "A complex history of subduction, back-arc basin formation, terrane accretion and transpressional shearing characterizes the evolution of the Caribbean and northern South American margin since Jurassic times. Quantitative plate tectonic reconstructions of the area do not include Jurassic-Cretaceous back-arc terranes of which there are both geological and geophysical observations. We developed a revised plate tectonic reconstruction based on geological observations and seismic tomography models to constrain the Jurassic-Cretaceous subduction history of eastern Panthalassa, along the western margin of the Caribbean region. This reconstruction considers the opening of a Northern Andean back-arc basin at 145 Ma, the Quebradagrande back-arc, closing at 120 Ma and followed by terrane accretion and northward translation along the South American margin starting at 100 Ma. This kinematic reconstruction is tested against two previously published tectonic reconstructions via coupling with global numerical mantle convection models using CitcomS. A comparison of modelled versus tomographically imaged mantle structure reveals that subduction outboard of the South American margin, lacking in previous tectonic models, is required to reproduce mid-mantle positive seismic anomalies imaged in P- and S-wave seismic tomography beneath South America, 500–2000 km in depth. Furthermore, we show that this subduction zone is likely produced by a back-arc basin that developed along the northern Andes during the Cretaceous via trench roll-back from 145 Ma and was closed at 100 Ma. The contemporaneous opening of the Quebradagrande back-arc basin with the Rocas Verdes back-arc basin in the southern Andes is consistent with a model that invokes return flow of mantle material behind a retreating slab and may explain why extension along the Peruvian and Chilean sections of the Andean margin did not experience full crustal break-up and back-arc opening during the late Jurassic-early Cretaceous Period." @default.
- W2890086380 created "2018-09-27" @default.
- W2890086380 creator A5011175371 @default.
- W2890086380 creator A5038326726 @default.
- W2890086380 creator A5042746575 @default.
- W2890086380 creator A5085624416 @default.
- W2890086380 date "2018-11-01" @default.
- W2890086380 modified "2023-10-16" @default.
- W2890086380 title "Geodynamic reconstruction of an accreted Cretaceous back-arc basin in the Northern Andes" @default.
- W2890086380 cites W1493790006 @default.
- W2890086380 cites W1504442666 @default.
- W2890086380 cites W1533198540 @default.
- W2890086380 cites W1544332985 @default.
- W2890086380 cites W1676343945 @default.
- W2890086380 cites W1890112748 @default.
- W2890086380 cites W1903967436 @default.
- W2890086380 cites W1944395750 @default.
- W2890086380 cites W1958675952 @default.
- W2890086380 cites W1965232766 @default.
- W2890086380 cites W1965738186 @default.
- W2890086380 cites W1968004466 @default.
- W2890086380 cites W1968367915 @default.
- W2890086380 cites W1969645733 @default.
- W2890086380 cites W1970892938 @default.
- W2890086380 cites W1977068211 @default.
- W2890086380 cites W1977369851 @default.
- W2890086380 cites W1979540100 @default.
- W2890086380 cites W1983132684 @default.
- W2890086380 cites W1986236153 @default.
- W2890086380 cites W1987786839 @default.
- W2890086380 cites W1990498673 @default.
- W2890086380 cites W1990874762 @default.
- W2890086380 cites W1991640456 @default.
- W2890086380 cites W1993052821 @default.
- W2890086380 cites W1994719407 @default.
- W2890086380 cites W1994803893 @default.
- W2890086380 cites W1999214953 @default.
- W2890086380 cites W2003125685 @default.
- W2890086380 cites W2017598849 @default.
- W2890086380 cites W2020804284 @default.
- W2890086380 cites W2021027438 @default.
- W2890086380 cites W2022526297 @default.
- W2890086380 cites W2023294412 @default.
- W2890086380 cites W2026340904 @default.
- W2890086380 cites W2030437775 @default.
- W2890086380 cites W2032607611 @default.
- W2890086380 cites W2037812844 @default.
- W2890086380 cites W2038285129 @default.
- W2890086380 cites W2039475184 @default.
- W2890086380 cites W2045464939 @default.
- W2890086380 cites W2049732070 @default.
- W2890086380 cites W2052431885 @default.
- W2890086380 cites W2053758306 @default.
- W2890086380 cites W2055364427 @default.
- W2890086380 cites W2056950411 @default.
- W2890086380 cites W2065092571 @default.
- W2890086380 cites W2066711037 @default.
- W2890086380 cites W2070384913 @default.
- W2890086380 cites W2070782043 @default.
- W2890086380 cites W2079851859 @default.
- W2890086380 cites W2080235901 @default.
- W2890086380 cites W2081839958 @default.
- W2890086380 cites W2088282694 @default.
- W2890086380 cites W2088893481 @default.
- W2890086380 cites W2091489546 @default.
- W2890086380 cites W2095352961 @default.
- W2890086380 cites W2097126717 @default.
- W2890086380 cites W2099691575 @default.
- W2890086380 cites W2100653978 @default.
- W2890086380 cites W2101073217 @default.
- W2890086380 cites W2103953314 @default.
- W2890086380 cites W2107780708 @default.
- W2890086380 cites W2109027182 @default.
- W2890086380 cites W2109518222 @default.
- W2890086380 cites W2111835129 @default.
- W2890086380 cites W2113390498 @default.
- W2890086380 cites W2116593025 @default.
- W2890086380 cites W2118197212 @default.
- W2890086380 cites W2118916526 @default.
- W2890086380 cites W2123823757 @default.
- W2890086380 cites W2124821889 @default.
- W2890086380 cites W2129333755 @default.
- W2890086380 cites W2137335718 @default.
- W2890086380 cites W2150872942 @default.
- W2890086380 cites W2152582070 @default.
- W2890086380 cites W2154463579 @default.
- W2890086380 cites W2154833867 @default.
- W2890086380 cites W2168593275 @default.
- W2890086380 cites W2170969682 @default.
- W2890086380 cites W2177277565 @default.
- W2890086380 cites W2178317302 @default.
- W2890086380 cites W2193455455 @default.
- W2890086380 cites W22404879 @default.
- W2890086380 cites W2289255802 @default.
- W2890086380 cites W2345939072 @default.
- W2890086380 cites W2569452410 @default.
- W2890086380 cites W2578487772 @default.
- W2890086380 cites W2593978807 @default.