FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2514277989> ?p ?o ?g. }

• W2514277989 abstract "The early Eocene Renegade Tongue of the Green River Formation in the Uinta basin, northeast Utah, is a fluvial siliciclastic dominated interval, interpreted as a fluvial megafan depositional system, interbedded with carbonate and siliciclastic lacustrine facies. Stratigraphy of the Green River Formation is poorly understood due to complex and variable spatial and temporal relationships between fluvial and lacustrine deposits. The complexity of these fluvial-lacustrine deposits is assigned to frequent climate-driven lake level fluctuations, as combined with longer-frequency allogenically controlled progradation and aggradation of the fluvial fans system, and lower-frequency autogenic processes, such as fan lobe and channel avulsions. Through the analysis of detailed outcrop measured sections, photomosaics, and optical thin section microscopy twenty two sedimentary facies and nine facies associations have been identified. These associations are grouped into fluvial, deltaic and lacustrine associations based on lateral and vertical facies association relationships. The fluvial associations include: FA 1.1 Amalgamated channels, FA 1.2 Isolated channels, FA 1.3 Tabular splay sandstones, and FA 1.4 Floodplain mudstones and siltstones. The deltaic associations include: FA 2.1 Distributary channels and mouth bars, FA 2.2 Tabular delta front turbidites, and FA 2.3 Prodelta mudstones and siltstones. The lacustrine carbonate associations include: FA 3.1 High energy lacustrine carbonates, and FA 3.2 Low energy lacustrine carbonates and microbialites. This study combines a detailed dataset across a triangle of three measured sections, each approximately one kilometer apart, in Nine Mile Canyon, Utah, with sub-regional scale correlations across approximately 130 kilometers. The detailed facies and facies associations provide a better understanding of vertical trends, lateral variability, and correlation of the fluvial, deltaic, and lacustrine complexities within the Renegade Tongue. In understanding this variability, intervals of allogenic and autogenic changes have been identified in correlations and complexity of the interaction between fluvial, deltaic, and lacustrine deposition was illustrated in 3D paleogeography time slices. The descriptions and interpretations of the interval can be compared with other fluvial intervals within the Uinta basin or across the globe, which provide valuable insights into the variability observable in other fluvio-lacustrine interfaces." @default.
• W2514277989 created "2016-09-16" @default.
• W2514277989 creator A5061463053 @default.
• W2514277989 date "2016-06-21" @default.
• W2514277989 modified "2023-09-22" @default.
• W2514277989 title "Complex fluvio-lacustrine stratigraphic interactions in the Renegade Tongue, Green River Formation, Uinta Basin, Utah" @default.
• W2514277989 cites W101633874 @default.
• W2514277989 cites W1508251117 @default.
• W2514277989 cites W1513519065 @default.
• W2514277989 cites W1536264477 @default.
• W2514277989 cites W1578437763 @default.
• W2514277989 cites W1585030024 @default.
• W2514277989 cites W1820830827 @default.
• W2514277989 cites W1848379162 @default.
• W2514277989 cites W1866189962 @default.
• W2514277989 cites W1907033508 @default.
• W2514277989 cites W1968164696 @default.
• W2514277989 cites W1972635099 @default.
• W2514277989 cites W1974536499 @default.
• W2514277989 cites W1976696102 @default.
• W2514277989 cites W2011204388 @default.
• W2514277989 cites W2027776215 @default.
• W2514277989 cites W2029712803 @default.
• W2514277989 cites W2030659127 @default.
• W2514277989 cites W2046654411 @default.
• W2514277989 cites W2049964887 @default.
• W2514277989 cites W2056542719 @default.
• W2514277989 cites W2057171595 @default.
• W2514277989 cites W2060728320 @default.
• W2514277989 cites W2063078603 @default.
• W2514277989 cites W2073111541 @default.
• W2514277989 cites W2077053821 @default.
• W2514277989 cites W2080453552 @default.
• W2514277989 cites W2087749178 @default.
• W2514277989 cites W2088829314 @default.
• W2514277989 cites W2097089409 @default.
• W2514277989 cites W2099512080 @default.
• W2514277989 cites W2101753605 @default.
• W2514277989 cites W2106272789 @default.
• W2514277989 cites W2117559107 @default.
• W2514277989 cites W2125981652 @default.
• W2514277989 cites W2132272817 @default.
• W2514277989 cites W2134756636 @default.
• W2514277989 cites W2135776977 @default.
• W2514277989 cites W2138659760 @default.
• W2514277989 cites W2138691699 @default.
• W2514277989 cites W2154846975 @default.
• W2514277989 cites W2157438953 @default.
• W2514277989 cites W2157509621 @default.
• W2514277989 cites W2162053709 @default.
• W2514277989 cites W2164625060 @default.
• W2514277989 cites W2231375138 @default.
• W2514277989 cites W2497643401 @default.
• W2514277989 cites W2912954225 @default.
• W2514277989 cites W2608665410 @default.
• W2514277989 hasPublicationYear "2016" @default.
• W2514277989 type Work @default.
• W2514277989 sameAs 2514277989 @default.
• W2514277989 citedByCount "0" @default.
• W2514277989 crossrefType "dissertation" @default.
• W2514277989 hasAuthorship W2514277989A5061463053 @default.
• W2514277989 hasConcept C109007969 @default.
• W2514277989 hasConcept C112959462 @default.
• W2514277989 hasConcept C114793014 @default.
• W2514277989 hasConcept C126753816 @default.
• W2514277989 hasConcept C127313418 @default.
• W2514277989 hasConcept C142614818 @default.
• W2514277989 hasConcept C146588470 @default.
• W2514277989 hasConcept C151730666 @default.
• W2514277989 hasConcept C16565575 @default.
• W2514277989 hasConcept C169212394 @default.
• W2514277989 hasConcept C2776169166 @default.
• W2514277989 hasConcept C32552466 @default.
• W2514277989 hasConcept C6494504 @default.
• W2514277989 hasConcept C93257316 @default.
• W2514277989 hasConceptScore W2514277989C109007969 @default.
• W2514277989 hasConceptScore W2514277989C112959462 @default.
• W2514277989 hasConceptScore W2514277989C114793014 @default.
• W2514277989 hasConceptScore W2514277989C126753816 @default.
• W2514277989 hasConceptScore W2514277989C127313418 @default.
• W2514277989 hasConceptScore W2514277989C142614818 @default.
• W2514277989 hasConceptScore W2514277989C146588470 @default.
• W2514277989 hasConceptScore W2514277989C151730666 @default.
• W2514277989 hasConceptScore W2514277989C16565575 @default.
• W2514277989 hasConceptScore W2514277989C169212394 @default.
• W2514277989 hasConceptScore W2514277989C2776169166 @default.
• W2514277989 hasConceptScore W2514277989C32552466 @default.
• W2514277989 hasConceptScore W2514277989C6494504 @default.
• W2514277989 hasConceptScore W2514277989C93257316 @default.
• W2514277989 hasLocation W25142779891 @default.
• W2514277989 hasOpenAccess W2514277989 @default.
• W2514277989 hasPrimaryLocation W25142779891 @default.
• W2514277989 hasRelatedWork W1443000514 @default.
• W2514277989 hasRelatedWork W1485025492 @default.
• W2514277989 hasRelatedWork W1586123442 @default.
• W2514277989 hasRelatedWork W1965015674 @default.
• W2514277989 hasRelatedWork W1965662669 @default.
• W2514277989 hasRelatedWork W1979376846 @default.
• W2514277989 hasRelatedWork W1998965085 @default.
• W2514277989 hasRelatedWork W2000567261 @default.

• next