FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2013060894> ?p ?o ?g. }

• W2013060894 endingPage "16481" @default.
• W2013060894 startingPage "16461" @default.
• W2013060894 abstract "We use a fully coupled asymmetric dynamic finite element model to study interactions between thermomechanical behavior and surface processes during continental rift evolution. The model accounts for (1) nonlinear brittle‐elastic‐ductile rheology, layered lithological structure, and faulting; (2) heat transport and thermal buoyancy forces; and (3) “true” erosion and sedimentation (grid elements are eliminated and recreated). Faults are not predefined but are self‐localized; their distributions and geometry are model outputs, which provides new geologically sensible constraints on its validity. We test previous ideas on rift evolution based on numerical and analytical component theories (or individual parts) of our model. After demonstrating that our coupled model reproduces classic rift features, we then demonstrate that synrift surface processes result in enhanced lithospheric thinning and widening of the basin, so that the apparent stretching factors increase by a factor of 1.5–2. Sedimentation results not only in thermal but also in localized flexural weakening of the lithosphere, which locally compensates strengthening due to cooling. Erosion on the uplifted flanks produces local strengthening and rebound. Surface processes produce pressure gradients, which drive a ductile crustal flow that (1) provides a fast feedback with tectonic processes and controls subsidence rates and flank stability and (2) drives a secondary extension or compression and uplift on the late synrift/early postrift phase. Our results indicate that kinematic and dynamic rift models that ignore erosion may produce misleading results in many rifts. We reproduced and explained a number of enigmatic synrift phenomena, such as (1) polyphase subsidence provoked by switching of the level of necking between different competent lithological layers and (2) synrift and postrift stagnation and vertical accelerations unassociated with tectonic stress inversion or phase changes." @default.
• W2013060894 created "2016-06-24" @default.
• W2013060894 creator A5044157820 @default.
• W2013060894 creator A5076982872 @default.
• W2013060894 date "2001-08-10" @default.
• W2013060894 modified "2023-10-18" @default.
• W2013060894 title "Erosion and rheology controls on synrift and postrift evolution: Verifying old and new ideas using a fully coupled numerical model" @default.
• W2013060894 cites W1525851193 @default.
• W2013060894 cites W1561132610 @default.
• W2013060894 cites W1565340041 @default.
• W2013060894 cites W1597948644 @default.
• W2013060894 cites W1601592176 @default.
• W2013060894 cites W1601684190 @default.
• W2013060894 cites W1965590780 @default.
• W2013060894 cites W1971644445 @default.
• W2013060894 cites W1973991885 @default.
• W2013060894 cites W1975198858 @default.
• W2013060894 cites W1978493430 @default.
• W2013060894 cites W1981556880 @default.
• W2013060894 cites W1984633020 @default.
• W2013060894 cites W1986890268 @default.
• W2013060894 cites W1989693454 @default.
• W2013060894 cites W1990236123 @default.
• W2013060894 cites W1994323983 @default.
• W2013060894 cites W1994357427 @default.
• W2013060894 cites W1994635685 @default.
• W2013060894 cites W1995115331 @default.
• W2013060894 cites W2008338511 @default.
• W2013060894 cites W2014395417 @default.
• W2013060894 cites W2020286870 @default.
• W2013060894 cites W2023781184 @default.
• W2013060894 cites W2024008393 @default.
• W2013060894 cites W2025290470 @default.
• W2013060894 cites W2033357906 @default.
• W2013060894 cites W2034753142 @default.
• W2013060894 cites W2035207306 @default.
• W2013060894 cites W2051651324 @default.
• W2013060894 cites W2052907420 @default.
• W2013060894 cites W2059424462 @default.
• W2013060894 cites W2064172684 @default.
• W2013060894 cites W2065947578 @default.
• W2013060894 cites W2075770239 @default.
• W2013060894 cites W2075928876 @default.
• W2013060894 cites W2086885317 @default.
• W2013060894 cites W2087420979 @default.
• W2013060894 cites W2087515369 @default.
• W2013060894 cites W2089453388 @default.
• W2013060894 cites W2090059326 @default.
• W2013060894 cites W2092352873 @default.
• W2013060894 cites W2095334417 @default.
• W2013060894 cites W2097878449 @default.
• W2013060894 cites W2107766160 @default.
• W2013060894 cites W2123108841 @default.
• W2013060894 cites W2123574189 @default.
• W2013060894 cites W2126039538 @default.
• W2013060894 cites W2132964817 @default.
• W2013060894 cites W2138411584 @default.
• W2013060894 cites W2148674466 @default.
• W2013060894 cites W2164687304 @default.
• W2013060894 cites W2165275336 @default.
• W2013060894 cites W2572492584 @default.
• W2013060894 doi "https://doi.org/10.1029/2001jb000433" @default.
• W2013060894 hasPublicationYear "2001" @default.
• W2013060894 type Work @default.
• W2013060894 sameAs 2013060894 @default.
• W2013060894 citedByCount "185" @default.
• W2013060894 countsByYear W20130608942012 @default.
• W2013060894 countsByYear W20130608942013 @default.
• W2013060894 countsByYear W20130608942014 @default.
• W2013060894 countsByYear W20130608942015 @default.
• W2013060894 countsByYear W20130608942016 @default.
• W2013060894 countsByYear W20130608942017 @default.
• W2013060894 countsByYear W20130608942018 @default.
• W2013060894 countsByYear W20130608942019 @default.
• W2013060894 countsByYear W20130608942020 @default.
• W2013060894 countsByYear W20130608942021 @default.
• W2013060894 countsByYear W20130608942022 @default.
• W2013060894 countsByYear W20130608942023 @default.
• W2013060894 crossrefType "journal-article" @default.
• W2013060894 hasAuthorship W2013060894A5044157820 @default.
• W2013060894 hasAuthorship W2013060894A5076982872 @default.
• W2013060894 hasBestOaLocation W20130608941 @default.
• W2013060894 hasConcept C121332964 @default.
• W2013060894 hasConcept C123157820 @default.
• W2013060894 hasConcept C127313418 @default.
• W2013060894 hasConcept C151730666 @default.
• W2013060894 hasConcept C16942324 @default.
• W2013060894 hasConcept C50682988 @default.
• W2013060894 hasConcept C538625479 @default.
• W2013060894 hasConcept C57879066 @default.
• W2013060894 hasConcept C77928131 @default.
• W2013060894 hasConcept C8058405 @default.
• W2013060894 hasConceptScore W2013060894C121332964 @default.
• W2013060894 hasConceptScore W2013060894C123157820 @default.
• W2013060894 hasConceptScore W2013060894C127313418 @default.
• W2013060894 hasConceptScore W2013060894C151730666 @default.
• W2013060894 hasConceptScore W2013060894C16942324 @default.
• W2013060894 hasConceptScore W2013060894C50682988 @default.

• next