FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2803523253> ?p ?o ?g. }

• W2803523253 endingPage "222" @default.
• W2803523253 startingPage "222" @default.
• W2803523253 abstract "Types of organic matter and mineral associations and microstructures of shales can reflect the depositional mechanism and sedimentary environment. Therefore, analysis of organic matter and mineral associations is a prerequisite for research on fine-grained sedimentary rocks. Shales from the Eocene Shahejie Formation in the Dongying Sag of China were selected to classify their lithofacies and to investigate the characteristics of their organic matter and mineral associations. This analysis identified six lithofacies (e.g., laminated shales and massive mudstones); in all the lithofacies, clay minerals exhibit a positive correlation with detrital minerals, thus indicating that they were derived from the same source. The comprehensive analysis of mineral and organic matter associations reveals that detrital minerals were deposited with low-hydrogen index (HI) OM. The deposition of detrital minerals was mainly a physical process. Clay minerals can undergo deposition in one of two ways due to their surface charge: they can either aggregate with high-HI OM via chemical deposition, thus forming organic-rich laminae, or they can be deposited together with low-HI OM via physical deposition, thus forming clay-rich laminae or a massive matrix. Carbonate minerals, which often coexist with high-HI OM, are biological sediments. The analysis of the sedimentary characteristics of these organic matter and mineral associations indicates that the sedimentary processes differ between various lithofacies: e.g., the discontinuous laminated shale represents the product of biophysical processes. Differences in depositional mechanisms are also present in each sub-member. Therefore, it is important to analyze the properties of minerals and organic matter, as well as their associations, to more deeply understand the classification of lithofacies and the depositional processes of shales and mudstones." @default.
• W2803523253 created "2018-06-01" @default.
• W2803523253 creator A5012392316 @default.
• W2803523253 creator A5027813350 @default.
• W2803523253 creator A5044282395 @default.
• W2803523253 creator A5076072416 @default.
• W2803523253 creator A5083281746 @default.
• W2803523253 date "2018-05-23" @default.
• W2803523253 modified "2023-10-02" @default.
• W2803523253 title "Relationship between Mineral and Organic Matter in Shales: The Case of Shahejie Formation, Dongying Sag, China" @default.
• W2803523253 cites W1970474696 @default.
• W2803523253 cites W1995340027 @default.
• W2803523253 cites W1995471679 @default.
• W2803523253 cites W2059022664 @default.
• W2803523253 cites W2067459493 @default.
• W2803523253 cites W2072094407 @default.
• W2803523253 cites W2084883729 @default.
• W2803523253 cites W2089973523 @default.
• W2803523253 cites W2148874527 @default.
• W2803523253 cites W2156037206 @default.
• W2803523253 cites W2166476646 @default.
• W2803523253 cites W2234228863 @default.
• W2803523253 cites W2341535003 @default.
• W2803523253 cites W2407613334 @default.
• W2803523253 cites W2473044071 @default.
• W2803523253 cites W2504675210 @default.
• W2803523253 cites W2573313702 @default.
• W2803523253 cites W2795358012 @default.
• W2803523253 doi "https://doi.org/10.3390/min8060222" @default.
• W2803523253 hasPublicationYear "2018" @default.
• W2803523253 type Work @default.
• W2803523253 sameAs 2803523253 @default.
• W2803523253 citedByCount "18" @default.
• W2803523253 countsByYear W28035232532019 @default.
• W2803523253 countsByYear W28035232532020 @default.
• W2803523253 countsByYear W28035232532021 @default.
• W2803523253 countsByYear W28035232532022 @default.
• W2803523253 countsByYear W28035232532023 @default.
• W2803523253 crossrefType "journal-article" @default.
• W2803523253 hasAuthorship W2803523253A5012392316 @default.
• W2803523253 hasAuthorship W2803523253A5027813350 @default.
• W2803523253 hasAuthorship W2803523253A5044282395 @default.
• W2803523253 hasAuthorship W2803523253A5076072416 @default.
• W2803523253 hasAuthorship W2803523253A5083281746 @default.
• W2803523253 hasBestOaLocation W28035232531 @default.
• W2803523253 hasConcept C109007969 @default.
• W2803523253 hasConcept C114793014 @default.
• W2803523253 hasConcept C126753816 @default.
• W2803523253 hasConcept C127313418 @default.
• W2803523253 hasConcept C130452526 @default.
• W2803523253 hasConcept C151730666 @default.
• W2803523253 hasConcept C153127940 @default.
• W2803523253 hasConcept C17409809 @default.
• W2803523253 hasConcept C178790620 @default.
• W2803523253 hasConcept C185592680 @default.
• W2803523253 hasConcept C199289684 @default.
• W2803523253 hasConcept C2776432453 @default.
• W2803523253 hasConcept C2779002002 @default.
• W2803523253 hasConcept C2780173749 @default.
• W2803523253 hasConcept C2780191791 @default.
• W2803523253 hasConcept C2816523 @default.
• W2803523253 hasConcept C40212044 @default.
• W2803523253 hasConcept C48743137 @default.
• W2803523253 hasConcept C64297162 @default.
• W2803523253 hasConcept C6494504 @default.
• W2803523253 hasConceptScore W2803523253C109007969 @default.
• W2803523253 hasConceptScore W2803523253C114793014 @default.
• W2803523253 hasConceptScore W2803523253C126753816 @default.
• W2803523253 hasConceptScore W2803523253C127313418 @default.
• W2803523253 hasConceptScore W2803523253C130452526 @default.
• W2803523253 hasConceptScore W2803523253C151730666 @default.
• W2803523253 hasConceptScore W2803523253C153127940 @default.
• W2803523253 hasConceptScore W2803523253C17409809 @default.
• W2803523253 hasConceptScore W2803523253C178790620 @default.
• W2803523253 hasConceptScore W2803523253C185592680 @default.
• W2803523253 hasConceptScore W2803523253C199289684 @default.
• W2803523253 hasConceptScore W2803523253C2776432453 @default.
• W2803523253 hasConceptScore W2803523253C2779002002 @default.
• W2803523253 hasConceptScore W2803523253C2780173749 @default.
• W2803523253 hasConceptScore W2803523253C2780191791 @default.
• W2803523253 hasConceptScore W2803523253C2816523 @default.
• W2803523253 hasConceptScore W2803523253C40212044 @default.
• W2803523253 hasConceptScore W2803523253C48743137 @default.
• W2803523253 hasConceptScore W2803523253C64297162 @default.
• W2803523253 hasConceptScore W2803523253C6494504 @default.
• W2803523253 hasIssue "6" @default.
• W2803523253 hasLocation W28035232531 @default.
• W2803523253 hasLocation W28035232532 @default.
• W2803523253 hasOpenAccess W2803523253 @default.
• W2803523253 hasPrimaryLocation W28035232531 @default.
• W2803523253 hasRelatedWork W121064149 @default.
• W2803523253 hasRelatedWork W1537989836 @default.
• W2803523253 hasRelatedWork W1971633880 @default.
• W2803523253 hasRelatedWork W1979075196 @default.
• W2803523253 hasRelatedWork W2017555201 @default.
• W2803523253 hasRelatedWork W2034759637 @default.
• W2803523253 hasRelatedWork W2045971906 @default.
• W2803523253 hasRelatedWork W2054854600 @default.

• next