FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3157830902> ?p ?o ?g. }

• W3157830902 endingPage "3115" @default.
• W3157830902 startingPage "3102" @default.
• W3157830902 abstract "Abstract Limestone–marl alternations are commonly used for high‐resolution cyclostratigraphic studies and palaeoenvironmental reconstructions, but diagenetic studies indicate that not all limestone–marl alternations reflect genuine differences in the initial sediment composition driven by environmental changes. Differences in the ratios of diagenetically inert trace elements between limestones and marls indicate changes affecting the terrigenous fraction of the precursor sediment. Contrarily, limestone–marl alternations without these differences can be the product of: (i) variations in CaCO 3 input (aragonite, calcite); (ii) distortion of the latter by diagenetic CaCO 3 redistribution; or (iii) diagenetic CaCO 3 redistribution in a homogeneous precursor sediment. The aim of this study is to provide a method to differentiate these cases and to identify variations in the proportion of calcite and aragonite in the precursor sediment composition. The model of differential diagenesis assumes that the concentration of diagenetically inert elements is inversely proportional to the amount of redistributed CaCO 3 . Consequently, the difference between ratios of diagenetically inert elements from two adjacent beds is a measure for CaCO 3 redistribution. This is quantifiable by the vector length between ratios from two adjacent beds. The approach is illustrated here by evaluation of a case study from the Silurian of Gotland, Sweden. Trace elements were compared according to their solubility during diagenesis. All elements bound to clay minerals or calcite show similar patterns of vector length, while vector length of elements which fit into the aragonite lattice, and are diagenetically mobile, differ. The vector length approach provides a tool to test the diagenetic origin of limestone–marl alternations, to identify initial variations in CaCO 3 input and to test a limestone–marl alternation’s suitability for cyclostratigraphic analyses." @default.
• W3157830902 created "2021-05-10" @default.
• W3157830902 creator A5011272953 @default.
• W3157830902 creator A5059786661 @default.
• W3157830902 creator A5065725878 @default.
• W3157830902 creator A5080795909 @default.
• W3157830902 date "2021-05-28" @default.
• W3157830902 modified "2023-09-27" @default.
• W3157830902 title "Detecting initial aragonite and calcite variations in limestone–marl alternations" @default.
• W3157830902 cites W1601650797 @default.
• W3157830902 cites W1813032990 @default.
• W3157830902 cites W1968692267 @default.
• W3157830902 cites W1971814833 @default.
• W3157830902 cites W1987208644 @default.
• W3157830902 cites W1988673802 @default.
• W3157830902 cites W2001156023 @default.
• W3157830902 cites W2014806185 @default.
• W3157830902 cites W2014933657 @default.
• W3157830902 cites W2018914060 @default.
• W3157830902 cites W2020247590 @default.
• W3157830902 cites W2025670111 @default.
• W3157830902 cites W2030026824 @default.
• W3157830902 cites W2046293644 @default.
• W3157830902 cites W2053818137 @default.
• W3157830902 cites W2054748909 @default.
• W3157830902 cites W2057391595 @default.
• W3157830902 cites W2058733983 @default.
• W3157830902 cites W2076327087 @default.
• W3157830902 cites W2087821779 @default.
• W3157830902 cites W2088240363 @default.
• W3157830902 cites W2120908352 @default.
• W3157830902 cites W2122226017 @default.
• W3157830902 cites W2133033835 @default.
• W3157830902 cites W2150113003 @default.
• W3157830902 cites W2156073122 @default.
• W3157830902 cites W2157423544 @default.
• W3157830902 cites W2221624887 @default.
• W3157830902 cites W2230218849 @default.
• W3157830902 cites W2268334776 @default.
• W3157830902 cites W2642833856 @default.
• W3157830902 cites W2793815292 @default.
• W3157830902 cites W2800756806 @default.
• W3157830902 cites W2910950270 @default.
• W3157830902 cites W2969565112 @default.
• W3157830902 cites W3120390351 @default.
• W3157830902 cites W4250485658 @default.
• W3157830902 cites W4385643468 @default.
• W3157830902 doi "https://doi.org/10.1111/sed.12885" @default.
• W3157830902 hasPublicationYear "2021" @default.
• W3157830902 type Work @default.
• W3157830902 sameAs 3157830902 @default.
• W3157830902 citedByCount "5" @default.
• W3157830902 countsByYear W31578309022022 @default.
• W3157830902 countsByYear W31578309022023 @default.
• W3157830902 crossrefType "journal-article" @default.
• W3157830902 hasAuthorship W3157830902A5011272953 @default.
• W3157830902 hasAuthorship W3157830902A5059786661 @default.
• W3157830902 hasAuthorship W3157830902A5065725878 @default.
• W3157830902 hasAuthorship W3157830902A5080795909 @default.
• W3157830902 hasBestOaLocation W31578309021 @default.
• W3157830902 hasConcept C109007969 @default.
• W3157830902 hasConcept C115393850 @default.
• W3157830902 hasConcept C127313418 @default.
• W3157830902 hasConcept C130452526 @default.
• W3157830902 hasConcept C151730666 @default.
• W3157830902 hasConcept C153018869 @default.
• W3157830902 hasConcept C17409809 @default.
• W3157830902 hasConcept C178790620 @default.
• W3157830902 hasConcept C185592680 @default.
• W3157830902 hasConcept C199289684 @default.
• W3157830902 hasConcept C2779866092 @default.
• W3157830902 hasConcept C2780191791 @default.
• W3157830902 hasConcept C2780659211 @default.
• W3157830902 hasConcept C2816523 @default.
• W3157830902 hasConcept C92927620 @default.
• W3157830902 hasConceptScore W3157830902C109007969 @default.
• W3157830902 hasConceptScore W3157830902C115393850 @default.
• W3157830902 hasConceptScore W3157830902C127313418 @default.
• W3157830902 hasConceptScore W3157830902C130452526 @default.
• W3157830902 hasConceptScore W3157830902C151730666 @default.
• W3157830902 hasConceptScore W3157830902C153018869 @default.
• W3157830902 hasConceptScore W3157830902C17409809 @default.
• W3157830902 hasConceptScore W3157830902C178790620 @default.
• W3157830902 hasConceptScore W3157830902C185592680 @default.
• W3157830902 hasConceptScore W3157830902C199289684 @default.
• W3157830902 hasConceptScore W3157830902C2779866092 @default.
• W3157830902 hasConceptScore W3157830902C2780191791 @default.
• W3157830902 hasConceptScore W3157830902C2780659211 @default.
• W3157830902 hasConceptScore W3157830902C2816523 @default.
• W3157830902 hasConceptScore W3157830902C92927620 @default.
• W3157830902 hasFunder F4320320879 @default.
• W3157830902 hasIssue "7" @default.
• W3157830902 hasLocation W31578309021 @default.
• W3157830902 hasLocation W315783090210 @default.
• W3157830902 hasLocation W31578309022 @default.
• W3157830902 hasLocation W31578309023 @default.
• W3157830902 hasLocation W31578309024 @default.
• W3157830902 hasLocation W31578309025 @default.

• next