FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2567353480> ?p ?o ?g. }

• W2567353480 endingPage "SD23" @default.
• W2567353480 startingPage "SD1" @default.
• W2567353480 abstract "Passive margins underlain by a salt detachment are typically interpreted as kinematically linked zones of updip extension and downdip contraction separated by a zone of translation above a smoothly dipping base of salt. However, salt flow is affected by the base-of-salt geometry across which it flows, and early-stage gravity gliding induced by basin tilt may be complicated by the presence of salt-thickness changes caused by the pre-existing base-salt relief. We investigate these effects using physical models. Dip-parallel steps generate strike-slip fault zones separating domains of differential downslope translation and structural styles, provided the overburden is thin enough. If the overburden is thicker, it resists breakup, but a change in the structural trend occurs across the step. Steps with mild obliquity to the dip direction produce transtensional and transpressional faults in the cover separating structural domains. Deformation complexity in the overburden increases where base-salt steps strike at a high angle to salt flow, and it is especially dependent on the ratio between the thick ([Formula: see text]) and thin ([Formula: see text]) salt across the step at the base of salt. Where the salt-thickness ratio ([Formula: see text]) is high, basal drag generates major flux mismatches, resulting in a contractional thickening of the salt and associated overburden shortening in thin salt above a base-salt high block. Shortening is transient and superseded by extension as the salt thickening allows the flow velocity to increase. When transitioning off a base-salt high block into a low block, the greater flux within the thick salt results in a monocline with extensional and contractional hinges. Structures are further deformed as they translate through these hinge zones. Our physical models demonstrate that extensional diapirs and compressional fold belts can be initiated anywhere on a slope as the salt accelerates and decelerates across base-salt relief. A fold belt from the Campos Basin, offshore Brazil, is used to illustrate these processes." @default.
• W2567353480 created "2017-01-06" @default.
• W2567353480 creator A5023187628 @default.
• W2567353480 creator A5027860588 @default.
• W2567353480 creator A5034218063 @default.
• W2567353480 creator A5048915841 @default.
• W2567353480 creator A5053621871 @default.
• W2567353480 date "2017-02-01" @default.
• W2567353480 modified "2023-10-18" @default.
• W2567353480 title "The effects of base-salt relief on salt flow and suprasalt deformation patterns — Part 1: Flow across simple steps in the base of salt" @default.
• W2567353480 cites W1970818142 @default.
• W2567353480 cites W1972370059 @default.
• W2567353480 cites W1999784638 @default.
• W2567353480 cites W2011864131 @default.
• W2567353480 cites W2024662598 @default.
• W2567353480 cites W2042296290 @default.
• W2567353480 cites W2056923231 @default.
• W2567353480 cites W2058198578 @default.
• W2567353480 cites W2062544518 @default.
• W2567353480 cites W2066021973 @default.
• W2567353480 cites W2073317479 @default.
• W2567353480 cites W2083690047 @default.
• W2567353480 cites W2088504567 @default.
• W2567353480 cites W2098687576 @default.
• W2567353480 cites W2100351772 @default.
• W2567353480 cites W2116548959 @default.
• W2567353480 cites W2125176922 @default.
• W2567353480 cites W2134109970 @default.
• W2567353480 cites W2135477555 @default.
• W2567353480 cites W2323049190 @default.
• W2567353480 cites W2494787865 @default.
• W2567353480 cites W2567353480 @default.
• W2567353480 doi "https://doi.org/10.1190/int-2016-0087.1" @default.
• W2567353480 hasPublicationYear "2017" @default.
• W2567353480 type Work @default.
• W2567353480 sameAs 2567353480 @default.
• W2567353480 citedByCount "46" @default.
• W2567353480 countsByYear W25673534802017 @default.
• W2567353480 countsByYear W25673534802018 @default.
• W2567353480 countsByYear W25673534802019 @default.
• W2567353480 countsByYear W25673534802020 @default.
• W2567353480 countsByYear W25673534802021 @default.
• W2567353480 countsByYear W25673534802022 @default.
• W2567353480 countsByYear W25673534802023 @default.
• W2567353480 crossrefType "journal-article" @default.
• W2567353480 hasAuthorship W2567353480A5023187628 @default.
• W2567353480 hasAuthorship W2567353480A5027860588 @default.
• W2567353480 hasAuthorship W2567353480A5034218063 @default.
• W2567353480 hasAuthorship W2567353480A5048915841 @default.
• W2567353480 hasAuthorship W2567353480A5053621871 @default.
• W2567353480 hasBestOaLocation W25673534801 @default.
• W2567353480 hasConcept C109007969 @default.
• W2567353480 hasConcept C113007552 @default.
• W2567353480 hasConcept C114793014 @default.
• W2567353480 hasConcept C127313418 @default.
• W2567353480 hasConcept C134306372 @default.
• W2567353480 hasConcept C147789679 @default.
• W2567353480 hasConcept C185592680 @default.
• W2567353480 hasConcept C187320778 @default.
• W2567353480 hasConcept C199007388 @default.
• W2567353480 hasConcept C199289684 @default.
• W2567353480 hasConcept C2524010 @default.
• W2567353480 hasConcept C2776371256 @default.
• W2567353480 hasConcept C2777201227 @default.
• W2567353480 hasConcept C33923547 @default.
• W2567353480 hasConcept C42058472 @default.
• W2567353480 hasConcept C5900021 @default.
• W2567353480 hasConceptScore W2567353480C109007969 @default.
• W2567353480 hasConceptScore W2567353480C113007552 @default.
• W2567353480 hasConceptScore W2567353480C114793014 @default.
• W2567353480 hasConceptScore W2567353480C127313418 @default.
• W2567353480 hasConceptScore W2567353480C134306372 @default.
• W2567353480 hasConceptScore W2567353480C147789679 @default.
• W2567353480 hasConceptScore W2567353480C185592680 @default.
• W2567353480 hasConceptScore W2567353480C187320778 @default.
• W2567353480 hasConceptScore W2567353480C199007388 @default.
• W2567353480 hasConceptScore W2567353480C199289684 @default.
• W2567353480 hasConceptScore W2567353480C2524010 @default.
• W2567353480 hasConceptScore W2567353480C2776371256 @default.
• W2567353480 hasConceptScore W2567353480C2777201227 @default.
• W2567353480 hasConceptScore W2567353480C33923547 @default.
• W2567353480 hasConceptScore W2567353480C42058472 @default.
• W2567353480 hasConceptScore W2567353480C5900021 @default.
• W2567353480 hasIssue "1" @default.
• W2567353480 hasLocation W25673534801 @default.
• W2567353480 hasOpenAccess W2567353480 @default.
• W2567353480 hasPrimaryLocation W25673534801 @default.
• W2567353480 hasRelatedWork W1892492676 @default.
• W2567353480 hasRelatedWork W2034193725 @default.
• W2567353480 hasRelatedWork W2056453526 @default.
• W2567353480 hasRelatedWork W2094771151 @default.
• W2567353480 hasRelatedWork W2107780220 @default.
• W2567353480 hasRelatedWork W2152583689 @default.
• W2567353480 hasRelatedWork W2378717535 @default.
• W2567353480 hasRelatedWork W3119089278 @default.
• W2567353480 hasRelatedWork W4211013931 @default.
• W2567353480 hasRelatedWork W4321995800 @default.
• W2567353480 hasVolume "5" @default.

• next