FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2066562746> ?p ?o ?g. }

• W2066562746 endingPage "84" @default.
• W2066562746 startingPage "78" @default.
• W2066562746 abstract "Numerous studies using various proxies have been conducted to ascertain the temperature of the Archean ocean. If, as some of these investigations indicate, the Archean ocean was relatively hot, with a cooling trend through time to the Phanerozoic, this would have had consequences for sediment erosion, transport and deposition. Substantially higher surface temperatures would cause the viscosity of water, an important variable in defining flow hydrodynamics, to be lowered. In particular, less viscous water would have affected the development of current ripples. These are dependent on the existence of the laminar sublayer, as the sweeps of turbulent eddies impinging on this layer build small mounds that evolve into ripples. The laminar sublayer thins at higher temperatures allowing sand grains of smaller sizes to destroy it. At modern surface temperatures current ripples cannot form in coarse-grained sands, and if a hotter ocean existed in the Archean it would have inhibited current ripple formation in medium-grained sands, and possibly even fine-grained sands. Examination of numerous Neoarchean, deep-water, turbiditic successions in western Superior Province led to the realization that ripple cross-lamination is rare in all these units. As the formation of current ripples is dependent on: the flow depositing sediment of the proper grainsize, velocities in the appropriate range, and existence of a viscous sublayer, and the first two prerequisites were met during deposition from these decelerating turbidity currents, the existence of the viscous sublayer during the majority of flows must be questioned. The occurrence of current ripple cross-lamination in well exposed turbidites of the Neoarchean, McKellar Harbour Formation was quantified and found to be substantially less than the abundance of ripple cross-lamination present in Phanerozoic turbidites, indicating that the Neoarchean deep ocean may have been considerably warmer than the deep ocean of today." @default.
• W2066562746 created "2016-06-24" @default.
• W2066562746 creator A5045064202 @default.
• W2066562746 creator A5090526461 @default.
• W2066562746 date "2011-11-01" @default.
• W2066562746 modified "2023-10-03" @default.
• W2066562746 title "Neoarchean deep marine paleotemperature: Evidence from turbidite successions" @default.
• W2066562746 cites W1513807038 @default.
• W2066562746 cites W1854178506 @default.
• W2066562746 cites W1964399673 @default.
• W2066562746 cites W1968815179 @default.
• W2066562746 cites W1968964243 @default.
• W2066562746 cites W1970418159 @default.
• W2066562746 cites W1972441357 @default.
• W2066562746 cites W1973215781 @default.
• W2066562746 cites W1980406234 @default.
• W2066562746 cites W1986601098 @default.
• W2066562746 cites W1987288872 @default.
• W2066562746 cites W1994760366 @default.
• W2066562746 cites W1998517510 @default.
• W2066562746 cites W1998695976 @default.
• W2066562746 cites W2000744341 @default.
• W2066562746 cites W2001363398 @default.
• W2066562746 cites W2001922145 @default.
• W2066562746 cites W2007817677 @default.
• W2066562746 cites W2010269231 @default.
• W2066562746 cites W2015210102 @default.
• W2066562746 cites W2018790242 @default.
• W2066562746 cites W2022438793 @default.
• W2066562746 cites W2023263621 @default.
• W2066562746 cites W2023380041 @default.
• W2066562746 cites W2026127155 @default.
• W2066562746 cites W2034414859 @default.
• W2066562746 cites W2047660877 @default.
• W2066562746 cites W2050474635 @default.
• W2066562746 cites W2054641948 @default.
• W2066562746 cites W2059398718 @default.
• W2066562746 cites W2060970030 @default.
• W2066562746 cites W2066230963 @default.
• W2066562746 cites W2071474926 @default.
• W2066562746 cites W2073019245 @default.
• W2066562746 cites W2073158252 @default.
• W2066562746 cites W2078817169 @default.
• W2066562746 cites W2079528230 @default.
• W2066562746 cites W2084016511 @default.
• W2066562746 cites W2084340623 @default.
• W2066562746 cites W2086248999 @default.
• W2066562746 cites W2089645746 @default.
• W2066562746 cites W2091171602 @default.
• W2066562746 cites W2091345565 @default.
• W2066562746 cites W2091610853 @default.
• W2066562746 cites W2096395977 @default.
• W2066562746 cites W2099093517 @default.
• W2066562746 cites W2100579964 @default.
• W2066562746 cites W2103189634 @default.
• W2066562746 cites W2104621823 @default.
• W2066562746 cites W2120935731 @default.
• W2066562746 cites W2121120480 @default.
• W2066562746 cites W2125489927 @default.
• W2066562746 cites W2131443336 @default.
• W2066562746 cites W2145685810 @default.
• W2066562746 cites W2146162221 @default.
• W2066562746 cites W2151450119 @default.
• W2066562746 cites W2154652984 @default.
• W2066562746 cites W2158300544 @default.
• W2066562746 cites W2203660717 @default.
• W2066562746 cites W2204153565 @default.
• W2066562746 cites W2240156425 @default.
• W2066562746 cites W2279163189 @default.
• W2066562746 cites W4237574439 @default.
• W2066562746 cites W4241039983 @default.
• W2066562746 doi "https://doi.org/10.1016/j.precamres.2011.09.004" @default.
• W2066562746 hasPublicationYear "2011" @default.
• W2066562746 type Work @default.
• W2066562746 sameAs 2066562746 @default.
• W2066562746 citedByCount "16" @default.
• W2066562746 countsByYear W20665627462013 @default.
• W2066562746 countsByYear W20665627462015 @default.
• W2066562746 countsByYear W20665627462017 @default.
• W2066562746 countsByYear W20665627462018 @default.
• W2066562746 countsByYear W20665627462019 @default.
• W2066562746 countsByYear W20665627462020 @default.
• W2066562746 countsByYear W20665627462023 @default.
• W2066562746 crossrefType "journal-article" @default.
• W2066562746 hasAuthorship W2066562746A5045064202 @default.
• W2066562746 hasAuthorship W2066562746A5090526461 @default.
• W2066562746 hasConcept C109007969 @default.
• W2066562746 hasConcept C111368507 @default.
• W2066562746 hasConcept C114793014 @default.
• W2066562746 hasConcept C121332964 @default.
• W2066562746 hasConcept C126753816 @default.
• W2066562746 hasConcept C127313418 @default.
• W2066562746 hasConcept C148043351 @default.
• W2066562746 hasConcept C149347711 @default.
• W2066562746 hasConcept C157954998 @default.
• W2066562746 hasConcept C165801399 @default.
• W2066562746 hasConcept C166528214 @default.
• W2066562746 hasConcept C17409809 @default.

• next