FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3185659402> ?p ?o ?g. }

• W3185659402 endingPage "2861" @default.
• W3185659402 startingPage "2837" @default.
• W3185659402 abstract "Abstract Classic models of gravity‐driven salt tectonics commonly depict kinematically linked zones of overburden deformation, characterised by updip extension and downdip contraction, separated by a weakly deformed zone associated with downdip translation above a relatively smooth base‐salt surface. We use 2D and 3D seismic reflection and borehole data from the south‐central Campos Basin to show that these models fail to adequately capture the complex range of structural styles forming during salt‐detached gravity‐driven deformation above a rugose base‐salt surface. In the Campos Basin, the base‐salt is defined by broadly NE‐trending, margin‐parallel, generally seaward‐dipping ramps that have up to 2 km of structural relief. We define three domains of overburden deformation: an updip extensional domain, an intermediate multiphase domain and a downdip contractional domain. The multiphase domain is defined by large, partly fault‐bounded, ramp‐syncline basins, the stratigraphic record of which suggest ca. 28 km of seaward gravity‐driven translation of salt and its overburden since the end of the Albian. We also identify three main types of salt structures in the multiphase domain: (a) contractional anticlines that were subjected to later extension and normal faulting; (b) passive‐to‐active diapirs that were later extended and widened, and which are bound on their landward margins by landward‐dipping, salt‐detached normal faults and (c) reactive (extensional) diapirs that were subsequently squeezed. We argue that this multiphase deformation occurs because of basinward translation of salt and its overburden over complex base‐salt relief, consistent with the predictions of physical models and several other seismic reflection data‐based studies. Critically, these complex local strains overprint margin‐scale patterns of deformation." @default.
• W3185659402 created "2021-08-02" @default.
• W3185659402 creator A5000563253 @default.
• W3185659402 creator A5001257543 @default.
• W3185659402 creator A5006938711 @default.
• W3185659402 creator A5009784381 @default.
• W3185659402 creator A5051782784 @default.
• W3185659402 date "2021-08-05" @default.
• W3185659402 modified "2023-10-18" @default.
• W3185659402 title "Pre‐salt rift morphology controls salt tectonics in the Campos Basin, offshore SE Brazil" @default.
• W3185659402 cites W1516314724 @default.
• W3185659402 cites W1599008295 @default.
• W3185659402 cites W1601770134 @default.
• W3185659402 cites W1973506630 @default.
• W3185659402 cites W1984434911 @default.
• W3185659402 cites W1986943807 @default.
• W3185659402 cites W1999784638 @default.
• W3185659402 cites W2004089187 @default.
• W3185659402 cites W2005878247 @default.
• W3185659402 cites W2012533964 @default.
• W3185659402 cites W2015460667 @default.
• W3185659402 cites W2016521458 @default.
• W3185659402 cites W2035208742 @default.
• W3185659402 cites W2035448021 @default.
• W3185659402 cites W2036536910 @default.
• W3185659402 cites W2047744596 @default.
• W3185659402 cites W2053035065 @default.
• W3185659402 cites W2056353799 @default.
• W3185659402 cites W2063807507 @default.
• W3185659402 cites W2065375137 @default.
• W3185659402 cites W2070667967 @default.
• W3185659402 cites W2075546878 @default.
• W3185659402 cites W2083690047 @default.
• W3185659402 cites W2105628276 @default.
• W3185659402 cites W2110585121 @default.
• W3185659402 cites W2112751836 @default.
• W3185659402 cites W2134109970 @default.
• W3185659402 cites W2135477555 @default.
• W3185659402 cites W2146634788 @default.
• W3185659402 cites W2146703019 @default.
• W3185659402 cites W2175821373 @default.
• W3185659402 cites W2312320724 @default.
• W3185659402 cites W2323049190 @default.
• W3185659402 cites W2516860937 @default.
• W3185659402 cites W2565719780 @default.
• W3185659402 cites W2589313355 @default.
• W3185659402 cites W2594123674 @default.
• W3185659402 cites W2604997487 @default.
• W3185659402 cites W2883604154 @default.
• W3185659402 cites W2922661896 @default.
• W3185659402 cites W2947100090 @default.
• W3185659402 cites W2962938715 @default.
• W3185659402 cites W2966040055 @default.
• W3185659402 cites W2996980263 @default.
• W3185659402 cites W3035002196 @default.
• W3185659402 cites W3097385514 @default.
• W3185659402 cites W3113443506 @default.
• W3185659402 cites W3119089278 @default.
• W3185659402 cites W3120996729 @default.
• W3185659402 cites W4246367839 @default.
• W3185659402 doi "https://doi.org/10.1111/bre.12588" @default.
• W3185659402 hasPublicationYear "2021" @default.
• W3185659402 type Work @default.
• W3185659402 sameAs 3185659402 @default.
• W3185659402 citedByCount "14" @default.
• W3185659402 countsByYear W31856594022021 @default.
• W3185659402 countsByYear W31856594022022 @default.
• W3185659402 countsByYear W31856594022023 @default.
• W3185659402 crossrefType "journal-article" @default.
• W3185659402 hasAuthorship W3185659402A5000563253 @default.
• W3185659402 hasAuthorship W3185659402A5001257543 @default.
• W3185659402 hasAuthorship W3185659402A5006938711 @default.
• W3185659402 hasAuthorship W3185659402A5009784381 @default.
• W3185659402 hasAuthorship W3185659402A5051782784 @default.
• W3185659402 hasBestOaLocation W31856594022 @default.
• W3185659402 hasConcept C109007969 @default.
• W3185659402 hasConcept C113007552 @default.
• W3185659402 hasConcept C114793014 @default.
• W3185659402 hasConcept C116637073 @default.
• W3185659402 hasConcept C127313418 @default.
• W3185659402 hasConcept C151730666 @default.
• W3185659402 hasConcept C155627805 @default.
• W3185659402 hasConcept C165205528 @default.
• W3185659402 hasConcept C199007388 @default.
• W3185659402 hasConcept C2777201227 @default.
• W3185659402 hasConcept C34221334 @default.
• W3185659402 hasConcept C5900021 @default.
• W3185659402 hasConcept C77928131 @default.
• W3185659402 hasConceptScore W3185659402C109007969 @default.
• W3185659402 hasConceptScore W3185659402C113007552 @default.
• W3185659402 hasConceptScore W3185659402C114793014 @default.
• W3185659402 hasConceptScore W3185659402C116637073 @default.
• W3185659402 hasConceptScore W3185659402C127313418 @default.
• W3185659402 hasConceptScore W3185659402C151730666 @default.
• W3185659402 hasConceptScore W3185659402C155627805 @default.
• W3185659402 hasConceptScore W3185659402C165205528 @default.
• W3185659402 hasConceptScore W3185659402C199007388 @default.
• W3185659402 hasConceptScore W3185659402C2777201227 @default.

• next