FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2066559968> ?p ?o ?g. }

• W2066559968 abstract "Abstract It is found that in the deepest part of Cooper Basin (Permian section in Nappamerri Trough) in South Australia, two shale formations, Roseneath and Murteree have potential to be shale gas reservoirs. However, a comprehensive petrophysical evaluation has not been carried out so far. The free porosity among minerals, pore throat geometry, surface area and structure of micro pores for adsorption and diffusion of gas in these formations have not been well understood. Two core samples from two wells (Della 4 and Moomba 46) were selected to evaluate mineralogy, free porosity and other petrophysical characterization. Since routine core analysis is not capable of petrophysical characterization of these very tight rocks, the latest technology of image scanning and processing of QEMSCAN (Quantitative Evaluation of Minerals using Scanning Electron Microscopy) and Computerized Tomography (CT) scanning have been used. QEMSCAN is a novel technology to process images from electron microscope to measure size and distribution of different minerals in a rock sample. QEMSCAN when combined with CT scanning can significantly enhance shale rock characterization and reservoir quality assessment. In this study, the main goal is the evaluation of total free porosity, micro pores and natural network of micro-fracture systems in our ultra fine samples. Based on QEMSCAN analysis, it is found that the sample of Murteree shale has the mineralogy of quartz 42.78%, siderite 6.75%, illite 28.96%, koalinite 14.09%, Total Organic Content (TOC) 1.91 wt%, and pyrite 0.04%, while rutile and other silicates minerals were identified as accessory minerals. Total free porosity is found to be 2 percent. The free porosity is largely associated with clay minerals which shows intergranular linear, isolated and elongated wedge shaped pores. SEM images from the same core sample also show that the pores are mainly present in clay rich zone. QEMSCAN maps have revealed the location of lamination, high and low porosity zones as well as high and low sorption areas. In CT scanning, the porosity found in QEMSCAN, was not identified; however, a network of micro-fracture system in Murteree shale sample is identified." @default.
• W2066559968 created "2016-06-24" @default.
• W2066559968 creator A5029584738 @default.
• W2066559968 creator A5032436780 @default.
• W2066559968 date "2012-10-22" @default.
• W2066559968 modified "2023-09-23" @default.
• W2066559968 title "Mineralogy and Petrophysical Evaluation of Roseneath and Murteree Shale Formations, Cooper Basin, Australia Using QEMSCAN and CT-Scanning" @default.
• W2066559968 cites W1976177815 @default.
• W2066559968 cites W1988607129 @default.
• W2066559968 cites W2007954148 @default.
• W2066559968 cites W2007975985 @default.
• W2066559968 cites W2018434255 @default.
• W2066559968 cites W2022696097 @default.
• W2066559968 cites W2063993373 @default.
• W2066559968 cites W2072613134 @default.
• W2066559968 cites W2077646803 @default.
• W2066559968 cites W2078202043 @default.
• W2066559968 cites W2134305838 @default.
• W2066559968 cites W2086277075 @default.
• W2066559968 doi "https://doi.org/10.2118/158461-ms" @default.
• W2066559968 hasPublicationYear "2012" @default.
• W2066559968 type Work @default.
• W2066559968 sameAs 2066559968 @default.
• W2066559968 citedByCount "4" @default.
• W2066559968 countsByYear W20665599682013 @default.
• W2066559968 countsByYear W20665599682015 @default.
• W2066559968 countsByYear W20665599682018 @default.
• W2066559968 countsByYear W20665599682019 @default.
• W2066559968 crossrefType "proceedings-article" @default.
• W2066559968 hasAuthorship W2066559968A5029584738 @default.
• W2066559968 hasAuthorship W2066559968A5032436780 @default.
• W2066559968 hasConcept C109007969 @default.
• W2066559968 hasConcept C127313418 @default.
• W2066559968 hasConcept C151730666 @default.
• W2066559968 hasConcept C153127940 @default.
• W2066559968 hasConcept C17409809 @default.
• W2066559968 hasConcept C187320778 @default.
• W2066559968 hasConcept C199289684 @default.
• W2066559968 hasConcept C46293882 @default.
• W2066559968 hasConcept C6648577 @default.
• W2066559968 hasConceptScore W2066559968C109007969 @default.
• W2066559968 hasConceptScore W2066559968C127313418 @default.
• W2066559968 hasConceptScore W2066559968C151730666 @default.
• W2066559968 hasConceptScore W2066559968C153127940 @default.
• W2066559968 hasConceptScore W2066559968C17409809 @default.
• W2066559968 hasConceptScore W2066559968C187320778 @default.
• W2066559968 hasConceptScore W2066559968C199289684 @default.
• W2066559968 hasConceptScore W2066559968C46293882 @default.
• W2066559968 hasConceptScore W2066559968C6648577 @default.
• W2066559968 hasLocation W20665599681 @default.
• W2066559968 hasOpenAccess W2066559968 @default.
• W2066559968 hasPrimaryLocation W20665599681 @default.
• W2066559968 hasRelatedWork W1976595108 @default.
• W2066559968 hasRelatedWork W2909358530 @default.
• W2066559968 hasRelatedWork W3137198918 @default.
• W2066559968 hasRelatedWork W789441901 @default.
• W2066559968 isParatext "false" @default.
• W2066559968 isRetracted "false" @default.
• W2066559968 magId "2066559968" @default.
• W2066559968 workType "article" @default.