Matches in SemOpenAlex for { <https://semopenalex.org/work/W2020307617> ?p ?o ?g. }
- W2020307617 endingPage "17" @default.
- W2020307617 startingPage "1" @default.
- W2020307617 abstract "The goal of this study was to determine the main factors that controlled the kinematic evolution and the structural architecture developed during the Late Triassic to Early Jurassic rifting that led to the opening of the Neuquén basin in the southwestern sector of Gondwana. We carried out a series of analog models to simulate an extensional system with a bent geometry similar to the northeastern border of the basin. In different experiments, we varied the extension direction between NNE (N10°E) and NE (N45°E) orientations, inducing rift systems with different degrees of obliquity in each sector of the extended area. We compared the kinematic evolution and the final structural architecture observed in the experiments with data from two selected representative areas of the basin: (1) the Atuel depocenter, situated in the northern Andean sector, and (2) the Entre Lomas area, situated in the northeastern Neuquén Embayment. In both cases, the good match between the field and subsurface data and the results of the analog models supports a NNE orientation of the regional extension (N30°E–N20°E) during the synrift stage. Our experimental results suggest that lithospheric weakness zones of NNW to NW trend could have controlled and localized the extension in the Neuquén basin. These previous anisotropies were linked to the sutures and rheological contrasts generated during the collision of terranes against the southwestern margin of Gondwana during the Paleozoic, as well as further modifications of the thermo-mechanical state of the lithosphere during the Late Paleozoic to Early Mesozoic evolution." @default.
- W2020307617 created "2016-06-24" @default.
- W2020307617 creator A5016652768 @default.
- W2020307617 creator A5023634822 @default.
- W2020307617 creator A5052854418 @default.
- W2020307617 creator A5075181834 @default.
- W2020307617 creator A5077905233 @default.
- W2020307617 creator A5089323069 @default.
- W2020307617 date "2014-09-01" @default.
- W2020307617 modified "2023-10-08" @default.
- W2020307617 title "Transtensional tectonics induced by oblique reactivation of previous lithospheric anisotropies during the Late Triassic to Early Jurassic rifting in the Neuquén basin: Insights from analog models" @default.
- W2020307617 cites W1512043619 @default.
- W2020307617 cites W1534673777 @default.
- W2020307617 cites W1629102058 @default.
- W2020307617 cites W1680566625 @default.
- W2020307617 cites W1965012680 @default.
- W2020307617 cites W1971103475 @default.
- W2020307617 cites W1974656229 @default.
- W2020307617 cites W1976433819 @default.
- W2020307617 cites W1977313794 @default.
- W2020307617 cites W1988004226 @default.
- W2020307617 cites W1988132814 @default.
- W2020307617 cites W1988993005 @default.
- W2020307617 cites W1989466398 @default.
- W2020307617 cites W1989655601 @default.
- W2020307617 cites W1997127647 @default.
- W2020307617 cites W1998252344 @default.
- W2020307617 cites W1999278873 @default.
- W2020307617 cites W2003382314 @default.
- W2020307617 cites W2003578564 @default.
- W2020307617 cites W2007996144 @default.
- W2020307617 cites W2008020474 @default.
- W2020307617 cites W2011864131 @default.
- W2020307617 cites W2013066991 @default.
- W2020307617 cites W2014560155 @default.
- W2020307617 cites W2019911729 @default.
- W2020307617 cites W2023796783 @default.
- W2020307617 cites W2024793243 @default.
- W2020307617 cites W2029869558 @default.
- W2020307617 cites W2031166321 @default.
- W2020307617 cites W2032456531 @default.
- W2020307617 cites W2032681444 @default.
- W2020307617 cites W2033911542 @default.
- W2020307617 cites W2034049221 @default.
- W2020307617 cites W2035216517 @default.
- W2020307617 cites W2038732125 @default.
- W2020307617 cites W2045173275 @default.
- W2020307617 cites W2045395616 @default.
- W2020307617 cites W2047754229 @default.
- W2020307617 cites W2048035806 @default.
- W2020307617 cites W2049209404 @default.
- W2020307617 cites W2062544518 @default.
- W2020307617 cites W2064803191 @default.
- W2020307617 cites W2065150191 @default.
- W2020307617 cites W2069716381 @default.
- W2020307617 cites W2075413468 @default.
- W2020307617 cites W2075910962 @default.
- W2020307617 cites W2077097585 @default.
- W2020307617 cites W2078464934 @default.
- W2020307617 cites W2080791398 @default.
- W2020307617 cites W2082412673 @default.
- W2020307617 cites W2086136946 @default.
- W2020307617 cites W2088000120 @default.
- W2020307617 cites W2091982998 @default.
- W2020307617 cites W2095352961 @default.
- W2020307617 cites W2105284409 @default.
- W2020307617 cites W2107544091 @default.
- W2020307617 cites W2115980374 @default.
- W2020307617 cites W2116130434 @default.
- W2020307617 cites W2118197212 @default.
- W2020307617 cites W2119560598 @default.
- W2020307617 cites W2121188225 @default.
- W2020307617 cites W2134607180 @default.
- W2020307617 cites W2148917252 @default.
- W2020307617 cites W2154745243 @default.
- W2020307617 cites W2154833867 @default.
- W2020307617 cites W2329748349 @default.
- W2020307617 cites W2467885025 @default.
- W2020307617 cites W2976749806 @default.
- W2020307617 cites W3129562778 @default.
- W2020307617 doi "https://doi.org/10.1016/j.jog.2014.04.010" @default.
- W2020307617 hasPublicationYear "2014" @default.
- W2020307617 type Work @default.
- W2020307617 sameAs 2020307617 @default.
- W2020307617 citedByCount "39" @default.
- W2020307617 countsByYear W20203076172015 @default.
- W2020307617 countsByYear W20203076172017 @default.
- W2020307617 countsByYear W20203076172018 @default.
- W2020307617 countsByYear W20203076172019 @default.
- W2020307617 countsByYear W20203076172020 @default.
- W2020307617 countsByYear W20203076172021 @default.
- W2020307617 countsByYear W20203076172022 @default.
- W2020307617 countsByYear W20203076172023 @default.
- W2020307617 crossrefType "journal-article" @default.
- W2020307617 hasAuthorship W2020307617A5016652768 @default.
- W2020307617 hasAuthorship W2020307617A5023634822 @default.
- W2020307617 hasAuthorship W2020307617A5052854418 @default.
- W2020307617 hasAuthorship W2020307617A5075181834 @default.