FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2327857587> ?p ?o ?g. }

• W2327857587 abstract "PreviousNext No Access12th International Congress of the Brazilian Geophysical Society & EXPOGEF, Rio de Janeiro, Brazil, 15–18 August 20113D HIGH RESOLUTION X-RAY COMPUTED MICROTOMOGRAPHY IN LIMESTONE ROCKS OF THE ITABORAÍ BASIN STUDIESAuthors: Milena F. S. OliveiraInaya LimaRicardo T. LopesLeonardo BorghiPaula FerrucioMilena F. S. OliveiraLaboratório de Instrumentação Nuclear (LIN), COPPE/UFRJSearch for more papers by this author, Inaya LimaLaboratório de Instrumentação Nuclear (LIN), COPPE/UFRJSearch for more papers by this author, Ricardo T. LopesLaboratório de Instrumentação Nuclear (LIN), COPPE/UFRJSearch for more papers by this author, Leonardo BorghiLaboratório de Geologia Sedimentar (LAGESED), IGEO/UFRJSearch for more papers by this author, and Paula Ferrucio(LPP) IGEO/UFRJSearch for more papers by this authorhttps://doi.org/10.1190/sbgf2011-309 SectionsAboutPDF/ePub ToolsAdd to favoritesDownload CitationsTrack CitationsPermissions ShareFacebookTwitterLinked InRedditEmail Abstract In this work it was studied core plugs from Itaborai basin that were collected in Sao Jose do Itaborai, Rio de Janeiro. This formation is characterized by carbonate sequence was covered by rudaceous sediments of Eocene-Oligocene age. This is a sequence of clastic and chemically deposited travertine limestones that were vertically cut by fissure. Understanding the size, connectivity and distribution of the pore space system is important for the reliable description of the basin petrophysical parameters. Conventional petrophysical techniques limit the observation in two dimensions and needs a special sample preparation. This work illustrates how the X ray computed microtomography (μ-CT) is able to study the 3D inner characteriscts of the pore space system with small resolution (~ microns order) and provide the 3D quantification of pores. It was studied samples of travertine limestone taken at different depths of the well called 2-ITAB-1-RJ. The results obtained show the potential of the μ-CT to describe the connectivity and distribution of pores from the 2D and 3D images and the 3D data porosity estimation. Keywords: rocks, high-resolution, microtomography, x rayPermalink: https://doi.org/10.1190/sbgf2011-309FiguresReferencesRelatedDetails 12th International Congress of the Brazilian Geophysical Society & EXPOGEF, Rio de Janeiro, Brazil, 15–18 August 2011ISSN (online):2159-6832Copyright: 2011 Pages: 2223 publication data© 2011 Published in electronic format with permission by the Brazilian Geophysical SocietyPublisher:Society of Exploration Geophysicists HistoryPublished: 13 Mar 2014 CITATION INFORMATION Milena F. S. Oliveira, Inaya Lima, Ricardo T. Lopes, Leonardo Borghi, and Paula Ferrucio, (2011), 3D HIGH RESOLUTION X-RAY COMPUTED MICROTOMOGRAPHY IN LIMESTONE ROCKS OF THE ITABORAÍ BASIN STUDIES, SEG Global Meeting Abstracts : 1498-1500. https://doi.org/10.1190/sbgf2011-309 Plain-Language Summary Keywordsrockshigh-resolutionmicrotomographyx rayPDF DownloadLoading ..." @default.
• W2327857587 created "2016-06-24" @default.
• W2327857587 creator A5010348148 @default.
• W2327857587 creator A5033809288 @default.
• W2327857587 creator A5058466945 @default.
• W2327857587 creator A5074927487 @default.
• W2327857587 creator A5086945846 @default.
• W2327857587 date "2011-03-13" @default.
• W2327857587 modified "2023-09-23" @default.
• W2327857587 title "3D HIGH RESOLUTION X-RAY COMPUTED MICROTOMOGRAPHY IN LIMESTONE ROCKS OF THE ITABORAÍ BASIN STUDIES" @default.
• W2327857587 cites W2098946957 @default.
• W2327857587 cites W2114123293 @default.
• W2327857587 doi "https://doi.org/10.1190/sbgf2011-309" @default.
• W2327857587 hasPublicationYear "2011" @default.
• W2327857587 type Work @default.
• W2327857587 sameAs 2327857587 @default.
• W2327857587 citedByCount "0" @default.
• W2327857587 crossrefType "proceedings-article" @default.
• W2327857587 hasAuthorship W2327857587A5010348148 @default.
• W2327857587 hasAuthorship W2327857587A5033809288 @default.
• W2327857587 hasAuthorship W2327857587A5058466945 @default.
• W2327857587 hasAuthorship W2327857587A5074927487 @default.
• W2327857587 hasAuthorship W2327857587A5086945846 @default.
• W2327857587 hasConcept C109007969 @default.
• W2327857587 hasConcept C114793014 @default.
• W2327857587 hasConcept C127313418 @default.
• W2327857587 hasConcept C138170599 @default.
• W2327857587 hasConcept C151730666 @default.
• W2327857587 hasConcept C169212394 @default.
• W2327857587 hasConcept C17409809 @default.
• W2327857587 hasConcept C187320778 @default.
• W2327857587 hasConcept C199289684 @default.
• W2327857587 hasConcept C3020199158 @default.
• W2327857587 hasConcept C46293882 @default.
• W2327857587 hasConcept C62649853 @default.
• W2327857587 hasConcept C6648577 @default.
• W2327857587 hasConceptScore W2327857587C109007969 @default.
• W2327857587 hasConceptScore W2327857587C114793014 @default.
• W2327857587 hasConceptScore W2327857587C127313418 @default.
• W2327857587 hasConceptScore W2327857587C138170599 @default.
• W2327857587 hasConceptScore W2327857587C151730666 @default.
• W2327857587 hasConceptScore W2327857587C169212394 @default.
• W2327857587 hasConceptScore W2327857587C17409809 @default.
• W2327857587 hasConceptScore W2327857587C187320778 @default.
• W2327857587 hasConceptScore W2327857587C199289684 @default.
• W2327857587 hasConceptScore W2327857587C3020199158 @default.
• W2327857587 hasConceptScore W2327857587C46293882 @default.
• W2327857587 hasConceptScore W2327857587C62649853 @default.
• W2327857587 hasConceptScore W2327857587C6648577 @default.
• W2327857587 hasLocation W23278575871 @default.
• W2327857587 hasOpenAccess W2327857587 @default.
• W2327857587 hasPrimaryLocation W23278575871 @default.
• W2327857587 hasRelatedWork W1547281 @default.
• W2327857587 hasRelatedWork W1547372024 @default.
• W2327857587 hasRelatedWork W1645446697 @default.
• W2327857587 hasRelatedWork W1902644217 @default.
• W2327857587 hasRelatedWork W1934834607 @default.
• W2327857587 hasRelatedWork W1997828999 @default.
• W2327857587 hasRelatedWork W2015969524 @default.
• W2327857587 hasRelatedWork W2107489490 @default.
• W2327857587 hasRelatedWork W2260644973 @default.
• W2327857587 hasRelatedWork W4206086527 @default.
• W2327857587 isParatext "false" @default.
• W2327857587 isRetracted "false" @default.
• W2327857587 magId "2327857587" @default.
• W2327857587 workType "article" @default.