FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2088892005> ?p ?o ?g. }

• W2088892005 endingPage "123" @default.
• W2088892005 startingPage "102" @default.
• W2088892005 abstract "Abstract Significant lateral variations in observed temperatures in the B eaufort‐ M ackenzie B asin raise the question on the temperature‐controlling factors. Based on the structural configuration of the sediments and underlying crust in the area, we calculate the steady‐state 3D conductive thermal field. Integrated data include the base of the relic permafrost layer representing the 0 °C‐isotherm, public‐domain temperature data (from 227 wells) and thermal conductivity data. For >75% of the wells the predicted temperatures deviate by <10 K from the observed temperatures, which validates the overall model setup and adopted thermal properties. One important trend reproduced by the model is a decrease in temperatures from the western to the eastern basin. While in the west, a maximum temperature of 185 °C is reached at 5000 m below sea level, in the east the maximum temperature is 138 °C. The main cause for this pattern lies in lateral variations in thermal conductivity indicating differences in the shale and sand contents of the different juxtaposed sedimentary units. North‐to‐south temperature trends reveal the superposition of deep and shallow effects. At the southern margin, where the insulating effect of the low‐conductive sediments is missing, temperatures are lowest. Farther north, where the sub‐sedimentary continental crust is thick enough to produce considerable heat and a thick pile of sediments efficiently stores heat, temperatures tend to be highest. Temperatures decrease again towards the northernmost distal parts of the basin, where thinned continental and oceanic crust produce less radiogenic heat. Wells with larger deviations of the purely conductive model from the temperature observations (>15 K at 10% of the wells) and their basin‐wide pattern of misfit tendency (too cold vs. too warm temperature predictions) point to a locally restricted coupling of heat transport to groundwater flow." @default.
• W2088892005 created "2016-06-24" @default.
• W2088892005 creator A5006634042 @default.
• W2088892005 creator A5064768807 @default.
• W2088892005 creator A5071780506 @default.
• W2088892005 creator A5090571465 @default.
• W2088892005 date "2014-07-10" @default.
• W2088892005 modified "2023-10-05" @default.
• W2088892005 title "Deep vs. shallow controlling factors of the crustal thermal field - insights from 3D modelling of the Beaufort-Mackenzie Basin (Arctic Canada)" @default.
• W2088892005 cites W1563894508 @default.
• W2088892005 cites W1964545035 @default.
• W2088892005 cites W1967371674 @default.
• W2088892005 cites W1971686709 @default.
• W2088892005 cites W1994454813 @default.
• W2088892005 cites W1998332950 @default.
• W2088892005 cites W2004407849 @default.
• W2088892005 cites W2013109133 @default.
• W2088892005 cites W2023641797 @default.
• W2088892005 cites W2024778669 @default.
• W2088892005 cites W2025841258 @default.
• W2088892005 cites W2032335138 @default.
• W2088892005 cites W2034977721 @default.
• W2088892005 cites W2038802627 @default.
• W2088892005 cites W2039365491 @default.
• W2088892005 cites W2042437692 @default.
• W2088892005 cites W2043043294 @default.
• W2088892005 cites W2044345773 @default.
• W2088892005 cites W2044656715 @default.
• W2088892005 cites W2051031036 @default.
• W2088892005 cites W2053078226 @default.
• W2088892005 cites W2053422754 @default.
• W2088892005 cites W2054978464 @default.
• W2088892005 cites W2061053358 @default.
• W2088892005 cites W2068216186 @default.
• W2088892005 cites W2074511487 @default.
• W2088892005 cites W2079428028 @default.
• W2088892005 cites W2080737167 @default.
• W2088892005 cites W2082462342 @default.
• W2088892005 cites W2086020452 @default.
• W2088892005 cites W2086980447 @default.
• W2088892005 cites W2091080771 @default.
• W2088892005 cites W2102313223 @default.
• W2088892005 cites W2106860441 @default.
• W2088892005 cites W2113772257 @default.
• W2088892005 cites W2115481049 @default.
• W2088892005 cites W2119249738 @default.
• W2088892005 cites W2123410601 @default.
• W2088892005 cites W2124173619 @default.
• W2088892005 cites W2129333755 @default.
• W2088892005 cites W2158468162 @default.
• W2088892005 cites W2159679817 @default.
• W2088892005 cites W2160163228 @default.
• W2088892005 cites W2161657613 @default.
• W2088892005 cites W2164312895 @default.
• W2088892005 cites W2166465211 @default.
• W2088892005 cites W2171374589 @default.
• W2088892005 cites W246761439 @default.
• W2088892005 cites W2791617759 @default.
• W2088892005 cites W2910138148 @default.
• W2088892005 cites W2910463918 @default.
• W2088892005 cites W2981860168 @default.
• W2088892005 cites W2981997860 @default.
• W2088892005 cites W2982070978 @default.
• W2088892005 cites W3022089344 @default.
• W2088892005 cites W4232328127 @default.
• W2088892005 cites W4234440840 @default.
• W2088892005 cites W4241935384 @default.
• W2088892005 cites W4254901490 @default.
• W2088892005 doi "https://doi.org/10.1111/bre.12075" @default.
• W2088892005 hasPublicationYear "2014" @default.
• W2088892005 type Work @default.
• W2088892005 sameAs 2088892005 @default.
• W2088892005 citedByCount "11" @default.
• W2088892005 countsByYear W20888920052016 @default.
• W2088892005 countsByYear W20888920052017 @default.
• W2088892005 countsByYear W20888920052018 @default.
• W2088892005 countsByYear W20888920052019 @default.
• W2088892005 countsByYear W20888920052020 @default.
• W2088892005 countsByYear W20888920052021 @default.
• W2088892005 countsByYear W20888920052022 @default.
• W2088892005 countsByYear W20888920052023 @default.
• W2088892005 crossrefType "journal-article" @default.
• W2088892005 hasAuthorship W2088892005A5006634042 @default.
• W2088892005 hasAuthorship W2088892005A5064768807 @default.
• W2088892005 hasAuthorship W2088892005A5071780506 @default.
• W2088892005 hasAuthorship W2088892005A5090571465 @default.
• W2088892005 hasConcept C109007969 @default.
• W2088892005 hasConcept C111368507 @default.
• W2088892005 hasConcept C114793014 @default.
• W2088892005 hasConcept C121332964 @default.
• W2088892005 hasConcept C127313418 @default.
• W2088892005 hasConcept C141646446 @default.
• W2088892005 hasConcept C15098985 @default.
• W2088892005 hasConcept C151730666 @default.
• W2088892005 hasConcept C16942324 @default.
• W2088892005 hasConcept C200646496 @default.
• W2088892005 hasConcept C2776698055 @default.
• W2088892005 hasConcept C2781451532 @default.

• next