FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1995395219> ?p ?o ?g. }

• W1995395219 endingPage "386" @default.
• W1995395219 startingPage "363" @default.
• W1995395219 abstract "Abstract The subsurface Oligocene Tikorangi Formation is a unique and important oil producer in the onshore Waihapa‐Ngaere Field, Taranaki Basin, being the only carbonate and fracture‐producing reservoir within the basin. Core sample data from seven onshore wells (foredeep megafacies) and a single offshore well (basinal megafacies) are correlated with a suite of sonic and gamma‐ray geophysical well log data to derive interpretative carbonate facies for the Tikorangi Formation. Four mixed siliciclastic ‐carbonate to carbonate facies have been defined: facies A— calcareous siliciclastite (<25% carbonate); facies B—very calcareous siliciclastite (25–50% carbonate); facies C— muddy limestone (50–75% carbonate); and facies D—coarse limestone (>75% carbonate). Single or interbedded combinations of these facies form the basis for identifying nine major lithostratigraphic units in the Tikorangi Formation that are correlatable between the eight wells in this study. The Tikorangi Formation accumulated across a shelf‐slope‐basin margin within a tectonically diversified basin setting, notably involving considerable off‐shelf redeposition of sediment into a bounding foredeep. Analysis of gamma, sonic, and resistivity well logs identifies five major episodes of sedimentary evolution. Episode I comprises re‐trogradational siliciclastic‐dominated redeposited units associated with foredeep subsidence. Episode II is a continuation of episode I retrogradation, but with increased mass‐redeposited carbonate influx during accelerated foredeep subsidence and relative sea‐level rise, the top marking the maximum flooding surface. Episode III involves a progradational sequence comprising relatively pure redeposited carbonate units associated with declining subsidence rates and minimal siliciclastic input, with movement of facies belts basinward. Episode IV consists of prograding aggradation involving essentially static facies belts dominated by often thick, periodically mass‐emplaced, carbonate‐rich units separated by thin background siliciclastic shale‐like units. Episode V is a retrogradational sequence marking the reintroduction of siliciclastic material into the basin following uplift of Mesozoic basement associated with accelerated compressional tectonics along the Australia‐Pacific plate boundary, initially diluting and ultimately extinguishing carbonate production factories and terminating deposition of the Tikorangi Formation." @default.
• W1995395219 created "2016-06-24" @default.
• W1995395219 creator A5001753624 @default.
• W1995395219 creator A5039271608 @default.
• W1995395219 creator A5070846497 @default.
• W1995395219 date "2003-09-01" @default.
• W1995395219 modified "2023-10-03" @default.
• W1995395219 title "Lithostratigraphy and depositional episodes of the Oligocene carbonate‐rich Tikorangi Formation, Taranaki Basin, New Zealand" @default.
• W1995395219 cites W11384943 @default.
• W1995395219 cites W1978157185 @default.
• W1995395219 cites W1985350839 @default.
• W1995395219 cites W1994011951 @default.
• W1995395219 cites W2012974174 @default.
• W1995395219 cites W2022366414 @default.
• W1995395219 cites W2023403646 @default.
• W1995395219 cites W2043399680 @default.
• W1995395219 cites W2078275838 @default.
• W1995395219 cites W2086655067 @default.
• W1995395219 cites W2103244224 @default.
• W1995395219 cites W2119395350 @default.
• W1995395219 cites W2126150865 @default.
• W1995395219 cites W2130950244 @default.
• W1995395219 cites W2155724780 @default.
• W1995395219 cites W2258985649 @default.
• W1995395219 cites W4236793099 @default.
• W1995395219 cites W4246157246 @default.
• W1995395219 cites W4250980847 @default.
• W1995395219 cites W635410625 @default.
• W1995395219 doi "https://doi.org/10.1080/00288306.2003.9515015" @default.
• W1995395219 hasPublicationYear "2003" @default.
• W1995395219 type Work @default.
• W1995395219 sameAs 1995395219 @default.
• W1995395219 citedByCount "22" @default.
• W1995395219 countsByYear W19953952192014 @default.
• W1995395219 countsByYear W19953952192018 @default.
• W1995395219 countsByYear W19953952192019 @default.
• W1995395219 countsByYear W19953952192020 @default.
• W1995395219 countsByYear W19953952192023 @default.
• W1995395219 crossrefType "journal-article" @default.
• W1995395219 hasAuthorship W1995395219A5001753624 @default.
• W1995395219 hasAuthorship W1995395219A5039271608 @default.
• W1995395219 hasAuthorship W1995395219A5070846497 @default.
• W1995395219 hasBestOaLocation W19953952192 @default.
• W1995395219 hasConcept C109007969 @default.
• W1995395219 hasConcept C126753816 @default.
• W1995395219 hasConcept C127313418 @default.
• W1995395219 hasConcept C146588470 @default.
• W1995395219 hasConcept C151730666 @default.
• W1995395219 hasConcept C17409809 @default.
• W1995395219 hasConcept C191897082 @default.
• W1995395219 hasConcept C192562407 @default.
• W1995395219 hasConcept C19320362 @default.
• W1995395219 hasConcept C2778609275 @default.
• W1995395219 hasConcept C2780659211 @default.
• W1995395219 hasConcept C42907665 @default.
• W1995395219 hasConcept C6494504 @default.
• W1995395219 hasConcept C93257316 @default.
• W1995395219 hasConceptScore W1995395219C109007969 @default.
• W1995395219 hasConceptScore W1995395219C126753816 @default.
• W1995395219 hasConceptScore W1995395219C127313418 @default.
• W1995395219 hasConceptScore W1995395219C146588470 @default.
• W1995395219 hasConceptScore W1995395219C151730666 @default.
• W1995395219 hasConceptScore W1995395219C17409809 @default.
• W1995395219 hasConceptScore W1995395219C191897082 @default.
• W1995395219 hasConceptScore W1995395219C192562407 @default.
• W1995395219 hasConceptScore W1995395219C19320362 @default.
• W1995395219 hasConceptScore W1995395219C2778609275 @default.
• W1995395219 hasConceptScore W1995395219C2780659211 @default.
• W1995395219 hasConceptScore W1995395219C42907665 @default.
• W1995395219 hasConceptScore W1995395219C6494504 @default.
• W1995395219 hasConceptScore W1995395219C93257316 @default.
• W1995395219 hasIssue "3" @default.
• W1995395219 hasLocation W19953952191 @default.
• W1995395219 hasLocation W19953952192 @default.
• W1995395219 hasOpenAccess W1995395219 @default.
• W1995395219 hasPrimaryLocation W19953952191 @default.
• W1995395219 hasRelatedWork W164419854 @default.
• W1995395219 hasRelatedWork W1995395219 @default.
• W1995395219 hasRelatedWork W2081758660 @default.
• W1995395219 hasRelatedWork W2123680436 @default.
• W1995395219 hasRelatedWork W2382377394 @default.
• W1995395219 hasRelatedWork W2888956007 @default.
• W1995395219 hasRelatedWork W3000923381 @default.
• W1995395219 hasRelatedWork W3133918748 @default.
• W1995395219 hasRelatedWork W3149875072 @default.
• W1995395219 hasRelatedWork W4324319422 @default.
• W1995395219 hasVolume "46" @default.
• W1995395219 isParatext "false" @default.
• W1995395219 isRetracted "false" @default.
• W1995395219 magId "1995395219" @default.
• W1995395219 workType "article" @default.