FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2560638882> ?p ?o ?g. }

• W2560638882 endingPage "253" @default.
• W2560638882 startingPage "243" @default.
• W2560638882 abstract "Despite the vast research on various aspects of its stratigraphy, relatively little is known about the source-rock potential of the Upper Jurassic Adriatic platform, southern Croatia. Here a case palynological study has been provided to determine the kerogen type, quality, and thermal maturity, and assess its relative hydrocarbon generative potential. Palynofacies characteristics indicate a low-energy, shallow-marine oxygen-depleted setting. The deposited mud-supported carbonates contain organic matter that is almost entirely composed of a fluorescent amorphous organic matter of planktonic and bacterial origin. A high phycomata/dinocyst ratio suggests relative hydrographic stability in an environment favorable for motile-stage dinoflagellate community with reduced production of dinocysts. The lack of anaerobic degradation and very good preservation of lipoid palynomorphs indicates dysoxic conditions; the latter also is suggested by a low proportion of algal-phytoplanktic carbohydrates. The lack of oxygen-deficient zone within the water column, coupled with well-preserved lipoid sediment components, suggests that the boundary between the oxygen-rich and oxygen-poor levels was likely located at/near the sediment-water interface. The palyno-organic facies analysis suggests that the organic matter corresponds to the type II (possibly I/II) kerogen (VRo ∼0.3–0.4%) that was protected from degradation before, during and after sedimentation. Well-preserved lipoid components suggest a good hydrocarbon-generative potential, but the low TOC values (<0.1%) of studied outcropping Upper Jurassic carbonates prevent their designation as source rocks. Given the known source-rock potential of the Upper Jurassic succession in the wider region, further studies of subsurface samples are needed to exclude the Oligocene-recent subaerial weathering as a culprit for the low TOC values." @default.
• W2560638882 created "2016-12-16" @default.
• W2560638882 creator A5000339513 @default.
• W2560638882 creator A5026871427 @default.
• W2560638882 creator A5046473843 @default.
• W2560638882 creator A5064466413 @default.
• W2560638882 date "2017-02-01" @default.
• W2560638882 modified "2023-09-27" @default.
• W2560638882 title "Palynofacies and paleoenvironment of the Upper Jurassic mud-supported carbonates, southern Croatia: Preliminary evaluation of the hydrocarbon source rock potential" @default.
• W2560638882 cites W1807528795 @default.
• W2560638882 cites W1885514292 @default.
• W2560638882 cites W1909115464 @default.
• W2560638882 cites W1922493939 @default.
• W2560638882 cites W1931739987 @default.
• W2560638882 cites W1983351619 @default.
• W2560638882 cites W1996873991 @default.
• W2560638882 cites W2007800496 @default.
• W2560638882 cites W2011076039 @default.
• W2560638882 cites W2016407557 @default.
• W2560638882 cites W2022634665 @default.
• W2560638882 cites W2023340085 @default.
• W2560638882 cites W2028241801 @default.
• W2560638882 cites W2037227996 @default.
• W2560638882 cites W2037509965 @default.
• W2560638882 cites W2049881046 @default.
• W2560638882 cites W2054704638 @default.
• W2560638882 cites W2055826656 @default.
• W2560638882 cites W2093779150 @default.
• W2560638882 cites W2104837834 @default.
• W2560638882 cites W2105027613 @default.
• W2560638882 cites W2113716498 @default.
• W2560638882 cites W2155472085 @default.
• W2560638882 cites W2171126358 @default.
• W2560638882 cites W2253067978 @default.
• W2560638882 cites W787689512 @default.
• W2560638882 doi "https://doi.org/10.1016/j.marpetgeo.2016.12.006" @default.
• W2560638882 hasPublicationYear "2017" @default.
• W2560638882 type Work @default.
• W2560638882 sameAs 2560638882 @default.
• W2560638882 citedByCount "9" @default.
• W2560638882 countsByYear W25606388822018 @default.
• W2560638882 countsByYear W25606388822021 @default.
• W2560638882 countsByYear W25606388822022 @default.
• W2560638882 countsByYear W25606388822023 @default.
• W2560638882 crossrefType "journal-article" @default.
• W2560638882 hasAuthorship W2560638882A5000339513 @default.
• W2560638882 hasAuthorship W2560638882A5026871427 @default.
• W2560638882 hasAuthorship W2560638882A5046473843 @default.
• W2560638882 hasAuthorship W2560638882A5064466413 @default.
• W2560638882 hasBestOaLocation W25606388821 @default.
• W2560638882 hasConcept C101433766 @default.
• W2560638882 hasConcept C109007969 @default.
• W2560638882 hasConcept C126559015 @default.
• W2560638882 hasConcept C126753816 @default.
• W2560638882 hasConcept C127313418 @default.
• W2560638882 hasConcept C138496976 @default.
• W2560638882 hasConcept C146588470 @default.
• W2560638882 hasConcept C151730666 @default.
• W2560638882 hasConcept C15744967 @default.
• W2560638882 hasConcept C162501224 @default.
• W2560638882 hasConcept C169212394 @default.
• W2560638882 hasConcept C17409809 @default.
• W2560638882 hasConcept C18903297 @default.
• W2560638882 hasConcept C2777678158 @default.
• W2560638882 hasConcept C2779196632 @default.
• W2560638882 hasConcept C2780618852 @default.
• W2560638882 hasConcept C2816523 @default.
• W2560638882 hasConcept C46984767 @default.
• W2560638882 hasConcept C48743137 @default.
• W2560638882 hasConcept C86803240 @default.
• W2560638882 hasConceptScore W2560638882C101433766 @default.
• W2560638882 hasConceptScore W2560638882C109007969 @default.
• W2560638882 hasConceptScore W2560638882C126559015 @default.
• W2560638882 hasConceptScore W2560638882C126753816 @default.
• W2560638882 hasConceptScore W2560638882C127313418 @default.
• W2560638882 hasConceptScore W2560638882C138496976 @default.
• W2560638882 hasConceptScore W2560638882C146588470 @default.
• W2560638882 hasConceptScore W2560638882C151730666 @default.
• W2560638882 hasConceptScore W2560638882C15744967 @default.
• W2560638882 hasConceptScore W2560638882C162501224 @default.
• W2560638882 hasConceptScore W2560638882C169212394 @default.
• W2560638882 hasConceptScore W2560638882C17409809 @default.
• W2560638882 hasConceptScore W2560638882C18903297 @default.
• W2560638882 hasConceptScore W2560638882C2777678158 @default.
• W2560638882 hasConceptScore W2560638882C2779196632 @default.
• W2560638882 hasConceptScore W2560638882C2780618852 @default.
• W2560638882 hasConceptScore W2560638882C2816523 @default.
• W2560638882 hasConceptScore W2560638882C46984767 @default.
• W2560638882 hasConceptScore W2560638882C48743137 @default.
• W2560638882 hasConceptScore W2560638882C86803240 @default.
• W2560638882 hasLocation W25606388821 @default.
• W2560638882 hasOpenAccess W2560638882 @default.
• W2560638882 hasPrimaryLocation W25606388821 @default.
• W2560638882 hasRelatedWork W2044025067 @default.
• W2560638882 hasRelatedWork W2378068645 @default.
• W2560638882 hasRelatedWork W2379560993 @default.
• W2560638882 hasRelatedWork W2941988457 @default.
• W2560638882 hasRelatedWork W2949711004 @default.

• next