FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1983896332> ?p ?o ?g. }

• W1983896332 endingPage "689" @default.
• W1983896332 startingPage "677" @default.
• W1983896332 abstract "Tectono-stratigraphic models of foredeep sedimentation have generally presumed a direct link between changing rates of tectonism and concomitant sedimentological response as manifested by change in thickness, composition or depositional environment of sediment accumulating in adjacent basins. Lacustrine limestone units within the early Cretaceous fluvial/lacustrine Gannett Group of western Wyoming exhibit systematic variation in several geochemical proxies of relative rates of precipitation and evaporation, indicating that lakewater chemistry was controlled by variation in regional climate. Change in proportion of allochthonous terrigenous clastic vs. autochthonous carbonate deposition, as well as carbonate Mg/Ca ratio and stable isotopic composition, occurs at two scales. Metre-scale alternation of micritic limestone and argillaceous marl is accompanied by mineralogical and isotopic variation within individual beds, indicating preferential carbonate accumulation during intervals of decreased regional meteoric precipitation relative to lake-surface evaporation. Limestone deposition began during intervals of maximum aridity, and decreased as increased meteoric precipitation-driven flux of terrigenous clastic sediment overwhelmed sites of carbonate accumulation. Similar upsection variation in limestone mineralogy and isotopic composition at a scale of tens of metres reflects the multiple processes of long-term increase in meteoric precipitation and lakewater freshening prior to influx of terrigenous sediment, across-basin fluvial-deltaic progradation, and renewed accumulation of riverine terrigenous units. Such trends suggest that formation-scale alternation between fluvial clastic and lacustrine carbonate deposition was controlled by climate change." @default.
• W1983896332 created "2016-06-24" @default.
• W1983896332 creator A5011975314 @default.
• W1983896332 creator A5040939030 @default.
• W1983896332 creator A5046191745 @default.
• W1983896332 date "1996-08-01" @default.
• W1983896332 modified "2023-10-18" @default.
• W1983896332 title "Climatic control of fluvial-lacustrine cyclicity in the Cretaceous Cordilleran Foreland Basin, western United States" @default.
• W1983896332 cites W151043946 @default.
• W1983896332 cites W1518673644 @default.
• W1983896332 cites W1970056623 @default.
• W1983896332 cites W1972070875 @default.
• W1983896332 cites W1974440507 @default.
• W1983896332 cites W1974767724 @default.
• W1983896332 cites W1986509574 @default.
• W1983896332 cites W1986516976 @default.
• W1983896332 cites W2000272155 @default.
• W1983896332 cites W2005649253 @default.
• W1983896332 cites W2006580400 @default.
• W1983896332 cites W2009537421 @default.
• W1983896332 cites W2010268246 @default.
• W1983896332 cites W2017807101 @default.
• W1983896332 cites W2035492077 @default.
• W1983896332 cites W2044460144 @default.
• W1983896332 cites W2045443252 @default.
• W1983896332 cites W2049218940 @default.
• W1983896332 cites W2057733284 @default.
• W1983896332 cites W2059849751 @default.
• W1983896332 cites W2063230287 @default.
• W1983896332 cites W2070846613 @default.
• W1983896332 cites W2074716904 @default.
• W1983896332 cites W2074906602 @default.
• W1983896332 cites W2081157532 @default.
• W1983896332 cites W2083239711 @default.
• W1983896332 cites W2090705149 @default.
• W1983896332 cites W2099512080 @default.
• W1983896332 cites W2111907446 @default.
• W1983896332 cites W2154355424 @default.
• W1983896332 cites W2157061841 @default.
• W1983896332 cites W2506550789 @default.
• W1983896332 cites W4211104829 @default.
• W1983896332 doi "https://doi.org/10.1111/j.1365-3091.1996.tb02020.x" @default.
• W1983896332 hasPublicationYear "1996" @default.
• W1983896332 type Work @default.
• W1983896332 sameAs 1983896332 @default.
• W1983896332 citedByCount "28" @default.
• W1983896332 countsByYear W19838963322013 @default.
• W1983896332 countsByYear W19838963322014 @default.
• W1983896332 countsByYear W19838963322016 @default.
• W1983896332 countsByYear W19838963322018 @default.
• W1983896332 countsByYear W19838963322019 @default.
• W1983896332 countsByYear W19838963322022 @default.
• W1983896332 countsByYear W19838963322023 @default.
• W1983896332 crossrefType "journal-article" @default.
• W1983896332 hasAuthorship W1983896332A5011975314 @default.
• W1983896332 hasAuthorship W1983896332A5040939030 @default.
• W1983896332 hasAuthorship W1983896332A5046191745 @default.
• W1983896332 hasBestOaLocation W19838963322 @default.
• W1983896332 hasConcept C109007969 @default.
• W1983896332 hasConcept C112959462 @default.
• W1983896332 hasConcept C126753816 @default.
• W1983896332 hasConcept C127313418 @default.
• W1983896332 hasConcept C138170599 @default.
• W1983896332 hasConcept C151730666 @default.
• W1983896332 hasConcept C17409809 @default.
• W1983896332 hasConcept C191897082 @default.
• W1983896332 hasConcept C192562407 @default.
• W1983896332 hasConcept C193748577 @default.
• W1983896332 hasConcept C199285206 @default.
• W1983896332 hasConcept C2780659211 @default.
• W1983896332 hasConcept C6494504 @default.
• W1983896332 hasConceptScore W1983896332C109007969 @default.
• W1983896332 hasConceptScore W1983896332C112959462 @default.
• W1983896332 hasConceptScore W1983896332C126753816 @default.
• W1983896332 hasConceptScore W1983896332C127313418 @default.
• W1983896332 hasConceptScore W1983896332C138170599 @default.
• W1983896332 hasConceptScore W1983896332C151730666 @default.
• W1983896332 hasConceptScore W1983896332C17409809 @default.
• W1983896332 hasConceptScore W1983896332C191897082 @default.
• W1983896332 hasConceptScore W1983896332C192562407 @default.
• W1983896332 hasConceptScore W1983896332C193748577 @default.
• W1983896332 hasConceptScore W1983896332C199285206 @default.
• W1983896332 hasConceptScore W1983896332C2780659211 @default.
• W1983896332 hasConceptScore W1983896332C6494504 @default.
• W1983896332 hasIssue "4" @default.
• W1983896332 hasLocation W19838963321 @default.
• W1983896332 hasLocation W19838963322 @default.
• W1983896332 hasOpenAccess W1983896332 @default.
• W1983896332 hasPrimaryLocation W19838963321 @default.
• W1983896332 hasRelatedWork W1586237999 @default.
• W1983896332 hasRelatedWork W1868012504 @default.
• W1983896332 hasRelatedWork W1996675075 @default.
• W1983896332 hasRelatedWork W2160728032 @default.
• W1983896332 hasRelatedWork W2365075172 @default.
• W1983896332 hasRelatedWork W2374062447 @default.
• W1983896332 hasRelatedWork W3034131340 @default.
• W1983896332 hasRelatedWork W3086570414 @default.
• W1983896332 hasRelatedWork W4282560349 @default.

• next