FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3162751668> ?p ?o ?g. }

• W3162751668 endingPage "105942" @default.
• W3162751668 startingPage "105942" @default.
• W3162751668 abstract "The Lower Ordovician mixed carbonate–shale Dumugol Formation of Korea was analysed to compare the stratal thickness and facies proportion of measured and decompacted successions and to assess the effect of compaction on the interpretation of cyclicity. Metre-scale cyclic units (MSUs) in the formation consist in part of outer-shelf shale, distal to intermediate mid-ramp limestone–shale couplets, and proximal mid-ramp lime mudstone facies. A total of 119 MSUs were recognised in the studied section. Thickness reduction was estimated based on petrographic evidence, including compressed to uncompressed burrows, firm- to hardground surfaces and differentially compacted laminae, and supplementary values of decompaction factors taken from the literature. Five oscillatory units in the apparent Fischer plots consist of thickening- to thinning-upward packages composed of shallowing- to deepening-upward MSUs. Similar thickness–facies relationships were observed in the lower two oscillatory units of the decompacted Fischer plots; these units are rich in shale. In contrast, a transition to an antithetic thickness–facies pattern occurs in the following units, with common occurrences of limestone facies. The different thickness–facies relationships in the measured and decompacted Dumugol successions indicate that a large portion of the major controls on the formation of sedimentary cyclicity changed from sediment accumulation rate to relative sea-level fluctuations. Such modification by compaction of the original sediment column appears to have been caused by early cementation in calcareous sediments, which resulted in differential thinning between limestone and shaly deposits. These findings reveal that diagenetic influences on sequence-stratigraphic and cyclostratigraphic interpretations have been underestimated, with consequent potential effects on associated local to regional geodynamic models, particularly for mixed carbonate–siliciclastic successions." @default.
• W3162751668 created "2021-05-24" @default.
• W3162751668 creator A5011826399 @default.
• W3162751668 creator A5067610707 @default.
• W3162751668 date "2021-07-01" @default.
• W3162751668 modified "2023-09-28" @default.
• W3162751668 title "Cyclic patterns in the Lower Ordovician Dumugol Formation, Korea: Influence of compaction on sequence-stratigraphic interpretation in mixed carbonate–shale successions" @default.
• W3162751668 cites W1033374690 @default.
• W3162751668 cites W1572053141 @default.
• W3162751668 cites W1851297183 @default.
• W3162751668 cites W1965375940 @default.
• W3162751668 cites W1972064005 @default.
• W3162751668 cites W1979717448 @default.
• W3162751668 cites W1982168560 @default.
• W3162751668 cites W1985866209 @default.
• W3162751668 cites W1987126212 @default.
• W3162751668 cites W1995253200 @default.
• W3162751668 cites W1996159800 @default.
• W3162751668 cites W1997206164 @default.
• W3162751668 cites W1997252211 @default.
• W3162751668 cites W1997691239 @default.
• W3162751668 cites W1998138507 @default.
• W3162751668 cites W2006081867 @default.
• W3162751668 cites W2006165788 @default.
• W3162751668 cites W2006395995 @default.
• W3162751668 cites W2016228000 @default.
• W3162751668 cites W2018804382 @default.
• W3162751668 cites W2021964852 @default.
• W3162751668 cites W2027532477 @default.
• W3162751668 cites W2027633350 @default.
• W3162751668 cites W2041373898 @default.
• W3162751668 cites W2043680455 @default.
• W3162751668 cites W2049935947 @default.
• W3162751668 cites W2052020844 @default.
• W3162751668 cites W2052346014 @default.
• W3162751668 cites W2052639207 @default.
• W3162751668 cites W2055245676 @default.
• W3162751668 cites W2059337784 @default.
• W3162751668 cites W2059509404 @default.
• W3162751668 cites W2061138879 @default.
• W3162751668 cites W2064571449 @default.
• W3162751668 cites W2072330338 @default.
• W3162751668 cites W2078740805 @default.
• W3162751668 cites W2080864796 @default.
• W3162751668 cites W2084183702 @default.
• W3162751668 cites W2085299338 @default.
• W3162751668 cites W2094807435 @default.
• W3162751668 cites W2105192118 @default.
• W3162751668 cites W2107802761 @default.
• W3162751668 cites W2111458329 @default.
• W3162751668 cites W2132300109 @default.
• W3162751668 cites W2132907539 @default.
• W3162751668 cites W2134178241 @default.
• W3162751668 cites W2145649605 @default.
• W3162751668 cites W2147427800 @default.
• W3162751668 cites W2153194713 @default.
• W3162751668 cites W2173350456 @default.
• W3162751668 cites W2186237828 @default.
• W3162751668 cites W2295821911 @default.
• W3162751668 cites W2296222902 @default.
• W3162751668 cites W2309765270 @default.
• W3162751668 cites W2332697542 @default.
• W3162751668 cites W2334002538 @default.
• W3162751668 cites W2490594183 @default.
• W3162751668 cites W2513057828 @default.
• W3162751668 cites W2522101507 @default.
• W3162751668 cites W2792096424 @default.
• W3162751668 cites W2794325795 @default.
• W3162751668 cites W2802159761 @default.
• W3162751668 cites W2898127214 @default.
• W3162751668 cites W2941100988 @default.
• W3162751668 cites W2943574525 @default.
• W3162751668 cites W2963806330 @default.
• W3162751668 cites W2964254036 @default.
• W3162751668 cites W3045872568 @default.
• W3162751668 cites W4237542223 @default.
• W3162751668 doi "https://doi.org/10.1016/j.sedgeo.2021.105942" @default.
• W3162751668 hasPublicationYear "2021" @default.
• W3162751668 type Work @default.
• W3162751668 sameAs 3162751668 @default.
• W3162751668 citedByCount "5" @default.
• W3162751668 countsByYear W31627516682022 @default.
• W3162751668 countsByYear W31627516682023 @default.
• W3162751668 crossrefType "journal-article" @default.
• W3162751668 hasAuthorship W3162751668A5011826399 @default.
• W3162751668 hasAuthorship W3162751668A5067610707 @default.
• W3162751668 hasConcept C109007969 @default.
• W3162751668 hasConcept C114793014 @default.
• W3162751668 hasConcept C126753816 @default.
• W3162751668 hasConcept C127313418 @default.
• W3162751668 hasConcept C130452526 @default.
• W3162751668 hasConcept C146588470 @default.
• W3162751668 hasConcept C151730666 @default.
• W3162751668 hasConcept C153018869 @default.
• W3162751668 hasConcept C153127940 @default.
• W3162751668 hasConcept C166957645 @default.
• W3162751668 hasConcept C17409809 @default.
• W3162751668 hasConcept C191897082 @default.

• next