FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2739894961> ?p ?o ?g. }

• W2739894961 abstract "High-CO2 gas fields serve as important analogues for understanding various processes related to CO2 injection and storage. The chemical signatures, both within the fluids and the solid phases, are especially useful for elucidating preferred gas migration pathways and also for assessing the relative importance of mineral dissolution and/or solution trapping efficiency. In this paper, we present a high resolution study focussed on the Gorgon gas field and associated Rankin trend gases on Australia’s Northwest Shelf of Australia. The Gorgon field is characterized by a series of stacked reservoirs (Figure 1), and is therefore well placed to characterize CO2 migration, dissolution and reaction by looking at geochemical signatures in the different reservoirs. Hydrological data at the Gorgon field also suggests that many of the major faults possess very low transmissivities, which should prevent or limit mixing of reservoir fluids with different chemical imprints. The gas data we present here reveal correlatable trends for mole %-CO2 and δ 13 C CO2 both areally and vertically as observed by Edwards et al. (2007). We suggest that the observed relationships are imparted due to mineral carbonation reactions that occurred along the CO2 migration pathway. These results have important implications for carbon storage operations and suggest that under certain conditions mineral sequestration might occur over longer migration distances and on shorter timescales than previously thought. The Australian NW shelf is a marginal rift setting which contains four basins, including the Carnarvon Basin. The Gorgon field, within the Carnarvon, is one of the largest gas fields in Australia (~ 40 TCF), with gases contained within an upthrown horst block defining the Rankin trend. Structurally, the Rankin horst block formed in response to late Triassic rifting, with later drowning of the system leading to formation of the intra Jurassic unconformity and deposition of the Muderong shale that forms the regional seal. The Rankin trend extends northward for more than a hundred kilometres to the Goodwyn and North Rankin fields. Gases of the Gorgon field are higher in CO2 than surrounding fields such as the Barrow Sub-basin and on the Exmouth Plateau. Currently it is believed that the CO2-rich Gorgon field gases migrated up and towards the southern Gorgon as a late dry charge and formed a spill chain to the north, displacing earlier, wetter gases (Longley et al, 2002). Gases of the Gorgon field have the highest CO2 concentrations among all gases in the Carnarvon Basin, with CO2 up to 16% and δ 13 C clustered between -3 to -5‰ (Figure 2). Within the Gorgon" @default.
• W2739894961 created "2017-08-08" @default.
• W2739894961 creator A5012201304 @default.
• W2739894961 creator A5021799785 @default.
• W2739894961 creator A5042066703 @default.
• W2739894961 creator A5089277700 @default.
• W2739894961 date "2010-01-01" @default.
• W2739894961 modified "2023-09-26" @default.
• W2739894961 title "Chemical Variations of CO2 in the Rankin Trend Natural Gases, Carnarvon Basin, Australia: An Example of Mineral Sequestration?" @default.
• W2739894961 cites W2033986829 @default.
• W2739894961 cites W2046109805 @default.
• W2739894961 cites W2276408133 @default.
• W2739894961 cites W2429260431 @default.
• W2739894961 hasPublicationYear "2010" @default.
• W2739894961 type Work @default.
• W2739894961 sameAs 2739894961 @default.
• W2739894961 citedByCount "0" @default.
• W2739894961 crossrefType "journal-article" @default.
• W2739894961 hasAuthorship W2739894961A5012201304 @default.
• W2739894961 hasAuthorship W2739894961A5021799785 @default.
• W2739894961 hasAuthorship W2739894961A5042066703 @default.
• W2739894961 hasAuthorship W2739894961A5089277700 @default.
• W2739894961 hasConcept C109007969 @default.
• W2739894961 hasConcept C111368507 @default.
• W2739894961 hasConcept C113740612 @default.
• W2739894961 hasConcept C120809312 @default.
• W2739894961 hasConcept C127313418 @default.
• W2739894961 hasConcept C132651083 @default.
• W2739894961 hasConcept C147789679 @default.
• W2739894961 hasConcept C151730666 @default.
• W2739894961 hasConcept C17409809 @default.
• W2739894961 hasConcept C178790620 @default.
• W2739894961 hasConcept C185592680 @default.
• W2739894961 hasConcept C1965285 @default.
• W2739894961 hasConcept C22884784 @default.
• W2739894961 hasConcept C2776432453 @default.
• W2739894961 hasConcept C2778379663 @default.
• W2739894961 hasConcept C50682988 @default.
• W2739894961 hasConcept C530467964 @default.
• W2739894961 hasConcept C59427239 @default.
• W2739894961 hasConcept C68189081 @default.
• W2739894961 hasConcept C88380143 @default.
• W2739894961 hasConceptScore W2739894961C109007969 @default.
• W2739894961 hasConceptScore W2739894961C111368507 @default.
• W2739894961 hasConceptScore W2739894961C113740612 @default.
• W2739894961 hasConceptScore W2739894961C120809312 @default.
• W2739894961 hasConceptScore W2739894961C127313418 @default.
• W2739894961 hasConceptScore W2739894961C132651083 @default.
• W2739894961 hasConceptScore W2739894961C147789679 @default.
• W2739894961 hasConceptScore W2739894961C151730666 @default.
• W2739894961 hasConceptScore W2739894961C17409809 @default.
• W2739894961 hasConceptScore W2739894961C178790620 @default.
• W2739894961 hasConceptScore W2739894961C185592680 @default.
• W2739894961 hasConceptScore W2739894961C1965285 @default.
• W2739894961 hasConceptScore W2739894961C22884784 @default.
• W2739894961 hasConceptScore W2739894961C2776432453 @default.
• W2739894961 hasConceptScore W2739894961C2778379663 @default.
• W2739894961 hasConceptScore W2739894961C50682988 @default.
• W2739894961 hasConceptScore W2739894961C530467964 @default.
• W2739894961 hasConceptScore W2739894961C59427239 @default.
• W2739894961 hasConceptScore W2739894961C68189081 @default.
• W2739894961 hasConceptScore W2739894961C88380143 @default.
• W2739894961 hasLocation W27398949611 @default.
• W2739894961 hasOpenAccess W2739894961 @default.
• W2739894961 hasPrimaryLocation W27398949611 @default.
• W2739894961 hasRelatedWork W1824040665 @default.
• W2739894961 hasRelatedWork W1981517515 @default.
• W2739894961 hasRelatedWork W1990256736 @default.
• W2739894961 hasRelatedWork W2069651016 @default.
• W2739894961 hasRelatedWork W2089722049 @default.
• W2739894961 hasRelatedWork W2120682162 @default.
• W2739894961 hasRelatedWork W2139836496 @default.
• W2739894961 hasRelatedWork W2156412639 @default.
• W2739894961 hasRelatedWork W2186320663 @default.
• W2739894961 hasRelatedWork W2200044695 @default.
• W2739894961 hasRelatedWork W2217183667 @default.
• W2739894961 hasRelatedWork W2272979381 @default.
• W2739894961 hasRelatedWork W2292583531 @default.
• W2739894961 hasRelatedWork W2347336010 @default.
• W2739894961 hasRelatedWork W2511838304 @default.
• W2739894961 hasRelatedWork W2980909525 @default.
• W2739894961 hasRelatedWork W2996752219 @default.
• W2739894961 hasRelatedWork W839104422 @default.
• W2739894961 hasRelatedWork W87101059 @default.
• W2739894961 hasRelatedWork W1890024815 @default.
• W2739894961 isParatext "false" @default.
• W2739894961 isRetracted "false" @default.
• W2739894961 magId "2739894961" @default.
• W2739894961 workType "article" @default.