FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1978249557> ?p ?o ?g. }

• W1978249557 endingPage "24" @default.
• W1978249557 startingPage "11" @default.
• W1978249557 abstract "Sedimentation coeval with growth of the Santaren anticline provides an excellent opportunity to study the relationships between sedimentation and anticline uplift through time. The Santaren anticline is a kilometre-scale, NW–SE trending fold offshore of Cuba, in the Bahamas foreland of the Cuban fold and thrust belt. The growth strata associated with this anticline consist of a thick package of carbonate sediments that were deposited without major interruptions from Neogene (and perhaps before) to present day. The excellent seismic resolution and age control of a number of seismic horizons within the growth strata allowed us to define 25 growth beds, each of them representing between 0.1 and 3.2 Ma. An analysis of the thickness of these beds allowed us to determine accurate quantitative values of cumulative decompacted thickness and crestal structural relief at the time of their deposition. In addition, for the same periods, sedimentation and fold uplift rates were calculated. Moreover, some information on relationships between sedimentation and fold uplift rates was inferred from the growth stratal geometry. Growth beds that overlap the fold crest and thin over it indicate that sedimentation rates outpaced fold growth rates during their deposition. Some overlapping beds have constant thickness indicating that no fold uplift occurred during their sedimentation. The rest of the growth beds exhibit onlap/offlap geometries that do not indicate a unique sedimentation/fold uplift rate relationship. Only in those cases in which the geometry of the underlying bed at the end of its deposition is known is it possible to infer a specific sedimentation/fold uplift rate relationship. As a result of this analysis, we have been able to (1) illustrate that the geometry of the growth strata associated with the Santaren anticline results from competition between sedimentation and tectonic fold uplift, (2) document the episodic and non-steady nature of fold growth, and (3) show that short-term rates (at the scale of hundreds of thousands years) provide much insight into the interplay between sedimentation and tectonic fold uplift that control the growth stratal patterns." @default.
• W1978249557 created "2016-06-24" @default.
• W1978249557 creator A5027264589 @default.
• W1978249557 creator A5027648877 @default.
• W1978249557 creator A5055820290 @default.
• W1978249557 creator A5058868778 @default.
• W1978249557 date "2002-01-01" @default.
• W1978249557 modified "2023-10-17" @default.
• W1978249557 title "Episodic folding inferred from syntectonic carbonate sedimentation: the Santaren anticline, Bahamas foreland" @default.
• W1978249557 cites W1963681023 @default.
• W1978249557 cites W1975067410 @default.
• W1978249557 cites W1986501104 @default.
• W1978249557 cites W1993454745 @default.
• W1978249557 cites W2001234864 @default.
• W1978249557 cites W2004399909 @default.
• W1978249557 cites W2021927142 @default.
• W1978249557 cites W2028528785 @default.
• W1978249557 cites W2030752458 @default.
• W1978249557 cites W2031480822 @default.
• W1978249557 cites W2041497525 @default.
• W1978249557 cites W2047326598 @default.
• W1978249557 cites W2054730724 @default.
• W1978249557 cites W2057490251 @default.
• W1978249557 cites W2065454109 @default.
• W1978249557 cites W2076779667 @default.
• W1978249557 cites W2094603286 @default.
• W1978249557 cites W2096557357 @default.
• W1978249557 cites W2097830317 @default.
• W1978249557 cites W2105808087 @default.
• W1978249557 cites W2120982838 @default.
• W1978249557 cites W2129192242 @default.
• W1978249557 cites W2133183611 @default.
• W1978249557 cites W2139868483 @default.
• W1978249557 cites W2140087217 @default.
• W1978249557 cites W2141627919 @default.
• W1978249557 cites W2142090258 @default.
• W1978249557 cites W2148799848 @default.
• W1978249557 cites W2151009515 @default.
• W1978249557 cites W2170619788 @default.
• W1978249557 cites W2403805344 @default.
• W1978249557 cites W2408266923 @default.
• W1978249557 doi "https://doi.org/10.1016/s0037-0738(01)00163-4" @default.
• W1978249557 hasPublicationYear "2002" @default.
• W1978249557 type Work @default.
• W1978249557 sameAs 1978249557 @default.
• W1978249557 citedByCount "39" @default.
• W1978249557 countsByYear W19782495572012 @default.
• W1978249557 countsByYear W19782495572014 @default.
• W1978249557 countsByYear W19782495572015 @default.
• W1978249557 countsByYear W19782495572016 @default.
• W1978249557 countsByYear W19782495572018 @default.
• W1978249557 countsByYear W19782495572019 @default.
• W1978249557 countsByYear W19782495572020 @default.
• W1978249557 countsByYear W19782495572021 @default.
• W1978249557 countsByYear W19782495572022 @default.
• W1978249557 countsByYear W19782495572023 @default.
• W1978249557 crossrefType "journal-article" @default.
• W1978249557 hasAuthorship W1978249557A5027264589 @default.
• W1978249557 hasAuthorship W1978249557A5027648877 @default.
• W1978249557 hasAuthorship W1978249557A5055820290 @default.
• W1978249557 hasAuthorship W1978249557A5058868778 @default.
• W1978249557 hasConcept C107058408 @default.
• W1978249557 hasConcept C114793014 @default.
• W1978249557 hasConcept C116637073 @default.
• W1978249557 hasConcept C127313418 @default.
• W1978249557 hasConcept C127413603 @default.
• W1978249557 hasConcept C151730666 @default.
• W1978249557 hasConcept C17409809 @default.
• W1978249557 hasConcept C191735495 @default.
• W1978249557 hasConcept C191897082 @default.
• W1978249557 hasConcept C192562407 @default.
• W1978249557 hasConcept C193748577 @default.
• W1978249557 hasConcept C2780659211 @default.
• W1978249557 hasConcept C2816523 @default.
• W1978249557 hasConcept C29941650 @default.
• W1978249557 hasConcept C53942344 @default.
• W1978249557 hasConcept C5900021 @default.
• W1978249557 hasConcept C6494504 @default.
• W1978249557 hasConcept C77928131 @default.
• W1978249557 hasConcept C78519656 @default.
• W1978249557 hasConceptScore W1978249557C107058408 @default.
• W1978249557 hasConceptScore W1978249557C114793014 @default.
• W1978249557 hasConceptScore W1978249557C116637073 @default.
• W1978249557 hasConceptScore W1978249557C127313418 @default.
• W1978249557 hasConceptScore W1978249557C127413603 @default.
• W1978249557 hasConceptScore W1978249557C151730666 @default.
• W1978249557 hasConceptScore W1978249557C17409809 @default.
• W1978249557 hasConceptScore W1978249557C191735495 @default.
• W1978249557 hasConceptScore W1978249557C191897082 @default.
• W1978249557 hasConceptScore W1978249557C192562407 @default.
• W1978249557 hasConceptScore W1978249557C193748577 @default.
• W1978249557 hasConceptScore W1978249557C2780659211 @default.
• W1978249557 hasConceptScore W1978249557C2816523 @default.
• W1978249557 hasConceptScore W1978249557C29941650 @default.
• W1978249557 hasConceptScore W1978249557C53942344 @default.
• W1978249557 hasConceptScore W1978249557C5900021 @default.
• W1978249557 hasConceptScore W1978249557C6494504 @default.
• W1978249557 hasConceptScore W1978249557C77928131 @default.

• next