FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2895909300> ?p ?o ?g. }

• W2895909300 endingPage "576" @default.
• W2895909300 startingPage "563" @default.
• W2895909300 abstract "3D seismic reflection data are used to investigate the processes which have led to the development of amplitude anomalies on reflectors in the faulted, Cenozoic overburden on the Laminaria High, Northwest Shelf of Australia. Amplitude and root mean square (RMS) attributes are mapped on two reflectors (seabed and horizon H9) that were deposited synchronous with fault activity and are located adjacent to predominantly ENE-WSW striking fault traces. On the seabed, the main anomaly is located on the up-dip side of the fault trace, and is elongated parallel to the local time structure contours. These observations are consistent with the anomalies having developed in response to structurally-controlled fluid seepage along, and up-dip migration away from the fault trace. The other amplitude anomalies associated with the H9 reflector are also located adjacent to fault traces but are discordant to the local time structure contours. The latter observation is inconsistent with the migration of buoyant fluid at the present day; instead, it suggests that the anomalies may be due to cemented hardgrounds that formed due to seepage when the faults intersected the palaeo-seafloor but were subsequently buried and deformed during ongoing sedimentation and fault growth/linkage. Prominent anomalies mapped on reflectors within the pre-faulting succession (H10) are located adjacent to, and are elongated along, sub-seismic scale, NW-SE striking faults or, as in the case of a deeper horizon (H13) show no clear relationship with the faults. We conclude that there is no relationship between the occurrence of anomalies and the magnitude of throw, or the duration of activity, along the Cenozoic faults. The results suggest that whilst fluid seepage and cementation were structurally-controlled, these processes were also influenced by permeability variations that cannot be resolved by seismic interpretation methods." @default.
• W2895909300 created "2018-10-26" @default.
• W2895909300 creator A5007928304 @default.
• W2895909300 creator A5030695421 @default.
• W2895909300 creator A5084059189 @default.
• W2895909300 date "2019-01-01" @default.
• W2895909300 modified "2023-10-09" @default.
• W2895909300 title "Geophysical evidence for structurally-controlled, authigenic carbonate cementation in the Laminaria High, Bonaparte basin, Northwest Shelf of Australia" @default.
• W2895909300 cites W1964062246 @default.
• W2895909300 cites W1981718144 @default.
• W2895909300 cites W1982210019 @default.
• W2895909300 cites W1985176283 @default.
• W2895909300 cites W1994600812 @default.
• W2895909300 cites W2003964127 @default.
• W2895909300 cites W2016213881 @default.
• W2895909300 cites W2038066120 @default.
• W2895909300 cites W2039488747 @default.
• W2895909300 cites W2053118815 @default.
• W2895909300 cites W2058697647 @default.
• W2895909300 cites W2061631377 @default.
• W2895909300 cites W2073411680 @default.
• W2895909300 cites W2076313493 @default.
• W2895909300 cites W2078026689 @default.
• W2895909300 cites W2083561174 @default.
• W2895909300 cites W2087066619 @default.
• W2895909300 cites W2106030949 @default.
• W2895909300 cites W2113203186 @default.
• W2895909300 cites W2245817976 @default.
• W2895909300 cites W2470557154 @default.
• W2895909300 cites W396343155 @default.
• W2895909300 doi "https://doi.org/10.1016/j.marpetgeo.2018.10.018" @default.
• W2895909300 hasPublicationYear "2019" @default.
• W2895909300 type Work @default.
• W2895909300 sameAs 2895909300 @default.
• W2895909300 citedByCount "2" @default.
• W2895909300 countsByYear W28959093002021 @default.
• W2895909300 crossrefType "journal-article" @default.
• W2895909300 hasAuthorship W2895909300A5007928304 @default.
• W2895909300 hasAuthorship W2895909300A5030695421 @default.
• W2895909300 hasAuthorship W2895909300A5084059189 @default.
• W2895909300 hasBestOaLocation W28959093002 @default.
• W2895909300 hasConcept C114793014 @default.
• W2895909300 hasConcept C115393850 @default.
• W2895909300 hasConcept C117485682 @default.
• W2895909300 hasConcept C127313418 @default.
• W2895909300 hasConcept C151730666 @default.
• W2895909300 hasConcept C165205528 @default.
• W2895909300 hasConcept C169212394 @default.
• W2895909300 hasConcept C175551986 @default.
• W2895909300 hasConcept C57803568 @default.
• W2895909300 hasConcept C6494504 @default.
• W2895909300 hasConceptScore W2895909300C114793014 @default.
• W2895909300 hasConceptScore W2895909300C115393850 @default.
• W2895909300 hasConceptScore W2895909300C117485682 @default.
• W2895909300 hasConceptScore W2895909300C127313418 @default.
• W2895909300 hasConceptScore W2895909300C151730666 @default.
• W2895909300 hasConceptScore W2895909300C165205528 @default.
• W2895909300 hasConceptScore W2895909300C169212394 @default.
• W2895909300 hasConceptScore W2895909300C175551986 @default.
• W2895909300 hasConceptScore W2895909300C57803568 @default.
• W2895909300 hasConceptScore W2895909300C6494504 @default.
• W2895909300 hasFunder F4320326118 @default.
• W2895909300 hasLocation W28959093001 @default.
• W2895909300 hasLocation W28959093002 @default.
• W2895909300 hasLocation W28959093003 @default.
• W2895909300 hasOpenAccess W2895909300 @default.
• W2895909300 hasPrimaryLocation W28959093001 @default.
• W2895909300 hasRelatedWork W183333406 @default.
• W2895909300 hasRelatedWork W2023753492 @default.
• W2895909300 hasRelatedWork W2045076813 @default.
• W2895909300 hasRelatedWork W2316627508 @default.
• W2895909300 hasRelatedWork W2320774206 @default.
• W2895909300 hasRelatedWork W2369558384 @default.
• W2895909300 hasRelatedWork W2384686665 @default.
• W2895909300 hasRelatedWork W2746583628 @default.
• W2895909300 hasRelatedWork W3217192627 @default.
• W2895909300 hasRelatedWork W4251927063 @default.
• W2895909300 hasVolume "99" @default.
• W2895909300 isParatext "false" @default.
• W2895909300 isRetracted "false" @default.
• W2895909300 magId "2895909300" @default.
• W2895909300 workType "article" @default.