FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2039795857> ?p ?o ?g. }

• W2039795857 endingPage "69" @default.
• W2039795857 startingPage "41" @default.
• W2039795857 abstract "The effects of high rates of subsidence and sediment supply, associated with orogenic uplift and loading, on the sequence-stratigraphic organization of two Middle Eocene, fan-delta clastic wedges on a foreland basin margin are highlighted. Specific topics addressed are: (1) the relevance of different key stratigraphic surfaces to the development of basic depositional cycles or sequences; (2) the stacking pattern of high-order sequences and the formation of lower-order composite sequences; (3) the time span and periodicity recorded by the sequence-hierarchy; (4) the traceability of coastal sequences into the alluvial realm; and (5) the relative importance of accommodation vs. sediment supply changes in controlling the sequence-hierarchy. Subaerial unconformities (and related lowstand systems tracts) developed in response to relative sea-level falls are generally not clearly recorded along the studied fan-delta clastic wedges, maybe because the rate of subsidence along this foreland margin exceeded the rate of falling eustatic sea level. The sequence stratigraphic approach used to subdivide these clastic wedges into repetitive, small-scale allostratigraphic units, or depositional cycles, is based on the recognition of transgressive–regressive (T–R) sequences (i.e. fundamental sequences), which are enveloped by a combination of shoreface ravinement and maximum regressive surfaces. Fundamental T–R sequences (3–80 m thick) are interpreted to record changes (with 104–105 year episodicities) in the rate of the terrigenous sediment supply to the shoreline. Systematic changes in the stacking pattern of the fundamental sequences define lower-order, T–R sequences of regional extent (i.e. composite sequences). These sequences (100–300 m thick) are interpreted to develop in response to nonperiodic 105–106 years episodicity, in the rate of sediment supply relative to the rate of accommodation creation. The stacking pattern of the successive composite sequences define a more than 1300 m thick T–R megasequence, which accumulated during a time span of ∼3 My, coeval with continuous thrusting activity. Increasing sediment supply rates through time, in response to the combination of a prevailing warm and humid climate and rapid tectonic uplift along the basin margin, controlled its internal T–R trend. The progressive increase in sediment supply initially compensated and eventually exceeded the increasing accommodation space created by both tectonic and sediment loading. The changing relative sea-level signals decayed and finally died away upstream from the coastal areas, as is evidenced by the fact that the T–R fundamental and composite sequences cannot be tied to the sequences recognized in the subaerial alluvial-fan domain. The latter appear to have been exclusively controlled by changes in the rate of sediment supply relative to the rate of subsidence change. This results in a clear coastal-to-alluvial sequence misfit." @default.
• W2039795857 created "2016-06-24" @default.
• W2039795857 creator A5010121776 @default.
• W2039795857 creator A5038715746 @default.
• W2039795857 creator A5049917384 @default.
• W2039795857 date "2000-12-01" @default.
• W2039795857 modified "2023-10-16" @default.
• W2039795857 title "Transgressive–regressive sequence hierarchy of foreland, fan-delta clastic wedges (Montserrat and Sant Llorenç del Munt, Middle Eocene, Ebro Basin, NE Spain)" @default.
• W2039795857 cites W1528030735 @default.
• W2039795857 cites W1964965246 @default.
• W2039795857 cites W1965846255 @default.
• W2039795857 cites W1986509574 @default.
• W2039795857 cites W1990100158 @default.
• W2039795857 cites W1997252211 @default.
• W2039795857 cites W2007721934 @default.
• W2039795857 cites W2012887763 @default.
• W2039795857 cites W2015218318 @default.
• W2039795857 cites W2032055224 @default.
• W2039795857 cites W2035856604 @default.
• W2039795857 cites W2043396789 @default.
• W2039795857 cites W2057385822 @default.
• W2039795857 cites W2057984754 @default.
• W2039795857 cites W2059195633 @default.
• W2039795857 cites W2059641633 @default.
• W2039795857 cites W2061858157 @default.
• W2039795857 cites W2074716904 @default.
• W2039795857 cites W2076093918 @default.
• W2039795857 cites W2076622177 @default.
• W2039795857 cites W2096557357 @default.
• W2039795857 cites W2098762071 @default.
• W2039795857 cites W2102264361 @default.
• W2039795857 cites W2119174036 @default.
• W2039795857 cites W2142301809 @default.
• W2039795857 cites W2152069662 @default.
• W2039795857 cites W2161761265 @default.
• W2039795857 cites W2318877923 @default.
• W2039795857 cites W2462206684 @default.
• W2039795857 doi "https://doi.org/10.1016/s0037-0738(00)00143-3" @default.
• W2039795857 hasPublicationYear "2000" @default.
• W2039795857 type Work @default.
• W2039795857 sameAs 2039795857 @default.
• W2039795857 citedByCount "51" @default.
• W2039795857 countsByYear W20397958572012 @default.
• W2039795857 countsByYear W20397958572013 @default.
• W2039795857 countsByYear W20397958572014 @default.
• W2039795857 countsByYear W20397958572016 @default.
• W2039795857 countsByYear W20397958572017 @default.
• W2039795857 countsByYear W20397958572018 @default.
• W2039795857 countsByYear W20397958572019 @default.
• W2039795857 countsByYear W20397958572020 @default.
• W2039795857 countsByYear W20397958572021 @default.
• W2039795857 crossrefType "journal-article" @default.
• W2039795857 hasAuthorship W2039795857A5010121776 @default.
• W2039795857 hasAuthorship W2039795857A5038715746 @default.
• W2039795857 hasAuthorship W2039795857A5049917384 @default.
• W2039795857 hasConcept C107058408 @default.
• W2039795857 hasConcept C109007969 @default.
• W2039795857 hasConcept C126753816 @default.
• W2039795857 hasConcept C127313418 @default.
• W2039795857 hasConcept C138170599 @default.
• W2039795857 hasConcept C151730666 @default.
• W2039795857 hasConcept C16565575 @default.
• W2039795857 hasConcept C193748577 @default.
• W2039795857 hasConcept C42907665 @default.
• W2039795857 hasConcept C6494504 @default.
• W2039795857 hasConceptScore W2039795857C107058408 @default.
• W2039795857 hasConceptScore W2039795857C109007969 @default.
• W2039795857 hasConceptScore W2039795857C126753816 @default.
• W2039795857 hasConceptScore W2039795857C127313418 @default.
• W2039795857 hasConceptScore W2039795857C138170599 @default.
• W2039795857 hasConceptScore W2039795857C151730666 @default.
• W2039795857 hasConceptScore W2039795857C16565575 @default.
• W2039795857 hasConceptScore W2039795857C193748577 @default.
• W2039795857 hasConceptScore W2039795857C42907665 @default.
• W2039795857 hasConceptScore W2039795857C6494504 @default.
• W2039795857 hasIssue "1-4" @default.
• W2039795857 hasLocation W20397958571 @default.
• W2039795857 hasOpenAccess W2039795857 @default.
• W2039795857 hasPrimaryLocation W20397958571 @default.
• W2039795857 hasRelatedWork W1586237999 @default.
• W2039795857 hasRelatedWork W1868012504 @default.
• W2039795857 hasRelatedWork W1991816519 @default.
• W2039795857 hasRelatedWork W1999273956 @default.
• W2039795857 hasRelatedWork W2057385822 @default.
• W2039795857 hasRelatedWork W2127255473 @default.
• W2039795857 hasRelatedWork W2167050352 @default.
• W2039795857 hasRelatedWork W2388852267 @default.
• W2039795857 hasRelatedWork W2793888850 @default.
• W2039795857 hasRelatedWork W3096577356 @default.
• W2039795857 hasVolume "138" @default.
• W2039795857 isParatext "false" @default.
• W2039795857 isRetracted "false" @default.
• W2039795857 magId "2039795857" @default.
• W2039795857 workType "article" @default.