FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2080656320> ?p ?o ?g. }

• W2080656320 endingPage "206" @default.
• W2080656320 startingPage "189" @default.
• W2080656320 abstract "Abstract The Western Kentucky Coal Field is the southern tip of the Eastern Interior, or Illinois Basin. Pennsylvanian rocks in this area, which include conglomerate, sandstone, siltstone, shale, limestone and coal, were deposited primarily in coastal-deltaic settings at a time when western Kentucky was located close to the equator. This paper discusses temporal changes in regional sedimentation patterns and coal-forming floras of Lower and Middle Pennsylvanian strata in the Western Kentucky Coal Field. Lower Pennsylvanian strata of the Caseyville Formation are characterized by paleovalley-filling sedimentation patterns and extabasinal quartz pebbles. Caseyville Formation coals are characteristically thin and discontinuous and were strongly influenced by subsidence within underlying paleovalleys, and the dissected lower Pennsylvanian paleotopography. Caseyville coals are commonly dominated by Lycospora, but can also have variable palynofloras, which probably reflects variable edaphic conditions and edge effects within small, patchy paleomires. Tradewater Formation strata show increased marine influences and tidal-estuarine sedimentation, especially in the middle and upper parts. Coal beds in the lower part of the Tradewater typically are thin and discontinuous, although some economically important beds are present. Coals become thicker, more abundant and more laterally persistent towards the top of the formation. Palynologically, lower and middle Tradewater Formation coals are dominated by Lycospora, but begin to show increased amounts of tree fern spores. Middle and upper Tradewater coals are thicker and more continuous, and contain high percentages of tree fern spores. In addition, cordaite pollen is locally abundant in this interval. Carbondale and Shelburn (Desmoinesian) strata are much more laterally continuous, and occur within classic cyclothems that can be traced across the coal field. Cyclothems have long been interpreted as being eustatically driven, and glacio-eustacy controlled not only sedimentation but also the formation of Desmoinesian paleomires. Palynologically, Carbondale and Shelburn coals are either dominated by Lycospora or have heterogeneous palynofloras. Palynologic and coal-quality data suggest that hydrologic base level may have been the primary control on Desmoinesian paleomires, rather than paleoclimate, as the coals display rheotrophic, rather than ombrotrophic characteristics." @default.
• W2080656320 created "2016-06-24" @default.
• W2080656320 creator A5039196540 @default.
• W2080656320 creator A5079274409 @default.
• W2080656320 creator A5080924012 @default.
• W2080656320 date "2001-07-01" @default.
• W2080656320 modified "2023-09-27" @default.
• W2080656320 title "The geology and palynology of Lower and Middle Pennsylvanian strata in the Western Kentucky Coal Field" @default.
• W2080656320 cites W2000648593 @default.
• W2080656320 cites W2004191809 @default.
• W2080656320 cites W2005124180 @default.
• W2080656320 cites W2008314211 @default.
• W2080656320 cites W2017593025 @default.
• W2080656320 cites W2021245952 @default.
• W2080656320 cites W2023637682 @default.
• W2080656320 cites W2033572198 @default.
• W2080656320 cites W2042594107 @default.
• W2080656320 cites W2044417994 @default.
• W2080656320 cites W2047958033 @default.
• W2080656320 cites W2052218531 @default.
• W2080656320 cites W2057416934 @default.
• W2080656320 cites W2058213822 @default.
• W2080656320 cites W2059231138 @default.
• W2080656320 cites W2064001311 @default.
• W2080656320 cites W2065290622 @default.
• W2080656320 cites W2065911477 @default.
• W2080656320 cites W2076261307 @default.
• W2080656320 doi "https://doi.org/10.1016/s0166-5162(01)00042-8" @default.
• W2080656320 hasPublicationYear "2001" @default.
• W2080656320 type Work @default.
• W2080656320 sameAs 2080656320 @default.
• W2080656320 citedByCount "28" @default.
• W2080656320 countsByYear W20806563202012 @default.
• W2080656320 countsByYear W20806563202013 @default.
• W2080656320 countsByYear W20806563202014 @default.
• W2080656320 countsByYear W20806563202016 @default.
• W2080656320 countsByYear W20806563202018 @default.
• W2080656320 countsByYear W20806563202019 @default.
• W2080656320 countsByYear W20806563202020 @default.
• W2080656320 countsByYear W20806563202021 @default.
• W2080656320 countsByYear W20806563202023 @default.
• W2080656320 crossrefType "journal-article" @default.
• W2080656320 hasAuthorship W2080656320A5039196540 @default.
• W2080656320 hasAuthorship W2080656320A5079274409 @default.
• W2080656320 hasAuthorship W2080656320A5080924012 @default.
• W2080656320 hasConcept C108615695 @default.
• W2080656320 hasConcept C109007969 @default.
• W2080656320 hasConcept C127313418 @default.
• W2080656320 hasConcept C151730666 @default.
• W2080656320 hasConcept C162501224 @default.
• W2080656320 hasConcept C16674752 @default.
• W2080656320 hasConcept C166957645 @default.
• W2080656320 hasConcept C17409809 @default.
• W2080656320 hasConcept C18903297 @default.
• W2080656320 hasConcept C205649164 @default.
• W2080656320 hasConcept C2779650180 @default.
• W2080656320 hasConcept C2780618852 @default.
• W2080656320 hasConcept C2994135397 @default.
• W2080656320 hasConcept C518851703 @default.
• W2080656320 hasConcept C86803240 @default.
• W2080656320 hasConceptScore W2080656320C108615695 @default.
• W2080656320 hasConceptScore W2080656320C109007969 @default.
• W2080656320 hasConceptScore W2080656320C127313418 @default.
• W2080656320 hasConceptScore W2080656320C151730666 @default.
• W2080656320 hasConceptScore W2080656320C162501224 @default.
• W2080656320 hasConceptScore W2080656320C16674752 @default.
• W2080656320 hasConceptScore W2080656320C166957645 @default.
• W2080656320 hasConceptScore W2080656320C17409809 @default.
• W2080656320 hasConceptScore W2080656320C18903297 @default.
• W2080656320 hasConceptScore W2080656320C205649164 @default.
• W2080656320 hasConceptScore W2080656320C2779650180 @default.
• W2080656320 hasConceptScore W2080656320C2780618852 @default.
• W2080656320 hasConceptScore W2080656320C2994135397 @default.
• W2080656320 hasConceptScore W2080656320C518851703 @default.
• W2080656320 hasConceptScore W2080656320C86803240 @default.
• W2080656320 hasIssue "3-4" @default.
• W2080656320 hasLocation W20806563201 @default.
• W2080656320 hasOpenAccess W2080656320 @default.
• W2080656320 hasPrimaryLocation W20806563201 @default.
• W2080656320 hasRelatedWork W1081763843 @default.
• W2080656320 hasRelatedWork W1606027898 @default.
• W2080656320 hasRelatedWork W1980952056 @default.
• W2080656320 hasRelatedWork W2015969524 @default.
• W2080656320 hasRelatedWork W2023042904 @default.
• W2080656320 hasRelatedWork W2210173755 @default.
• W2080656320 hasRelatedWork W2481149937 @default.
• W2080656320 hasRelatedWork W2844653506 @default.
• W2080656320 hasRelatedWork W2910494433 @default.
• W2080656320 hasRelatedWork W3100605844 @default.
• W2080656320 hasVolume "47" @default.
• W2080656320 isParatext "false" @default.
• W2080656320 isRetracted "false" @default.
• W2080656320 magId "2080656320" @default.
• W2080656320 workType "article" @default.