FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1993832306> ?p ?o ?g. }

• W1993832306 endingPage "602" @default.
• W1993832306 startingPage "581" @default.
• W1993832306 abstract "Dolomitization of platform carbonates is commonly the result of multiphase processes. Documentation of the complex dolomitization history is difficult if completely dolomitized sections are studied. Two Middle Anisian sections representing two coeval carbonate platforms were investigated and compared in the present study. Both sections are made up of meter-scale peritidal–lagoonal cycles with significant pedogenic overprint. One of the sections contains non-dolomitized, partially dolomitized, and completely dolomitized intervals, whereas the other is completely dolomitized. Based on investigations of the partially dolomitized section, penecontemporaneous dolomite formation and/or very early post-depositional dolomitization were identified in various lithofacies types. In shallow subtidal facies, porphyrotopic dolomite was found preferentially in microbial micritic fabrics. Microbially induced dolomite precipitation and/or progressive replacement of carbonate sediments could be interpreted for stromatolites. Cryptocrystalline to very finely crystalline dolomite, probably of pedogenic origin, was encountered in paleosoil horizons. Fabric-destructive dolomite commonly found below these horizons was likely formed via reflux of evaporated seawater. As a result of the different paleogeographic settings of the two platforms, their shallow-burial conditions were significantly different. One of the studied sections was located at the basinward platform margin where pervasive fabric-retentive dolomitization took place in a shallow-burial setting, probably via thermal convection. In contrast, in the area of the other, smaller platform shallow-water carbonates were covered by basinal deposits, preventing fluid circulation and accordingly pervasive shallow-burial dolomitization. In the intermediate to deep burial zone, recrystallization of partially dolomitized limestone and occlusion of newly opened fractures and pores by coarsely crystalline dolomite took place." @default.
• W1993832306 created "2016-06-24" @default.
• W1993832306 creator A5060162170 @default.
• W1993832306 creator A5067158282 @default.
• W1993832306 creator A5078472495 @default.
• W1993832306 creator A5084033936 @default.
• W1993832306 date "2014-02-23" @default.
• W1993832306 modified "2023-09-26" @default.
• W1993832306 title "Similarities and differences in the dolomitization history of two coeval Middle Triassic carbonate platforms, Balaton Highland, Hungary" @default.
• W1993832306 cites W1524701735 @default.
• W1993832306 cites W1563041753 @default.
• W1993832306 cites W1566908542 @default.
• W1993832306 cites W1575363025 @default.
• W1993832306 cites W1613337856 @default.
• W1993832306 cites W1943121318 @default.
• W1993832306 cites W1970316273 @default.
• W1993832306 cites W1989373718 @default.
• W1993832306 cites W1996137722 @default.
• W1993832306 cites W2013988132 @default.
• W1993832306 cites W2023547193 @default.
• W1993832306 cites W2026608718 @default.
• W1993832306 cites W2054222338 @default.
• W1993832306 cites W2062953728 @default.
• W1993832306 cites W2069767281 @default.
• W1993832306 cites W2069939822 @default.
• W1993832306 cites W2077568485 @default.
• W1993832306 cites W2078169777 @default.
• W1993832306 cites W2093817160 @default.
• W1993832306 cites W2095530176 @default.
• W1993832306 cites W2097627207 @default.
• W1993832306 cites W2118497769 @default.
• W1993832306 cites W2123936849 @default.
• W1993832306 cites W2135791232 @default.
• W1993832306 cites W2137439053 @default.
• W1993832306 cites W2142156816 @default.
• W1993832306 cites W2150772200 @default.
• W1993832306 cites W2156201366 @default.
• W1993832306 cites W2157294932 @default.
• W1993832306 cites W2168761377 @default.
• W1993832306 cites W2235226982 @default.
• W1993832306 cites W2895614241 @default.
• W1993832306 cites W3109625297 @default.
• W1993832306 cites W4244715764 @default.
• W1993832306 cites W4250980847 @default.
• W1993832306 doi "https://doi.org/10.1007/s10347-014-0397-1" @default.
• W1993832306 hasPublicationYear "2014" @default.
• W1993832306 type Work @default.
• W1993832306 sameAs 1993832306 @default.
• W1993832306 citedByCount "5" @default.
• W1993832306 countsByYear W19938323062014 @default.
• W1993832306 countsByYear W19938323062016 @default.
• W1993832306 countsByYear W19938323062017 @default.
• W1993832306 countsByYear W19938323062020 @default.
• W1993832306 countsByYear W19938323062022 @default.
• W1993832306 crossrefType "journal-article" @default.
• W1993832306 hasAuthorship W1993832306A5060162170 @default.
• W1993832306 hasAuthorship W1993832306A5067158282 @default.
• W1993832306 hasAuthorship W1993832306A5078472495 @default.
• W1993832306 hasAuthorship W1993832306A5084033936 @default.
• W1993832306 hasBestOaLocation W19938323062 @default.
• W1993832306 hasConcept C104873425 @default.
• W1993832306 hasConcept C109007969 @default.
• W1993832306 hasConcept C126753816 @default.
• W1993832306 hasConcept C127313418 @default.
• W1993832306 hasConcept C146588470 @default.
• W1993832306 hasConcept C151730666 @default.
• W1993832306 hasConcept C17409809 @default.
• W1993832306 hasConcept C191897082 @default.
• W1993832306 hasConcept C192562407 @default.
• W1993832306 hasConcept C1965285 @default.
• W1993832306 hasConcept C2776797426 @default.
• W1993832306 hasConcept C2778609275 @default.
• W1993832306 hasConcept C2780659211 @default.
• W1993832306 hasConcept C63662990 @default.
• W1993832306 hasConceptScore W1993832306C104873425 @default.
• W1993832306 hasConceptScore W1993832306C109007969 @default.
• W1993832306 hasConceptScore W1993832306C126753816 @default.
• W1993832306 hasConceptScore W1993832306C127313418 @default.
• W1993832306 hasConceptScore W1993832306C146588470 @default.
• W1993832306 hasConceptScore W1993832306C151730666 @default.
• W1993832306 hasConceptScore W1993832306C17409809 @default.
• W1993832306 hasConceptScore W1993832306C191897082 @default.
• W1993832306 hasConceptScore W1993832306C192562407 @default.
• W1993832306 hasConceptScore W1993832306C1965285 @default.
• W1993832306 hasConceptScore W1993832306C2776797426 @default.
• W1993832306 hasConceptScore W1993832306C2778609275 @default.
• W1993832306 hasConceptScore W1993832306C2780659211 @default.
• W1993832306 hasConceptScore W1993832306C63662990 @default.
• W1993832306 hasIssue "2" @default.
• W1993832306 hasLocation W19938323061 @default.
• W1993832306 hasLocation W19938323062 @default.
• W1993832306 hasOpenAccess W1993832306 @default.
• W1993832306 hasPrimaryLocation W19938323061 @default.
• W1993832306 hasRelatedWork W1992520171 @default.
• W1993832306 hasRelatedWork W1993832306 @default.
• W1993832306 hasRelatedWork W2015033492 @default.
• W1993832306 hasRelatedWork W2066216729 @default.
• W1993832306 hasRelatedWork W2102481219 @default.

• next