FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2055607114> ?p ?o ?g. }

• W2055607114 endingPage "104" @default.
• W2055607114 startingPage "91" @default.
• W2055607114 abstract "Deep, wide oceanic basins are the only regions of old seafloor where depth is truly representative of thermal isostasy. When the depths of these basins are corrected for the effect of sediment accumulation, and variation in crustal thickness, the principal non-thermal factors have been eliminated. We collect the most precise and reliable values of heat flow for the same basins, from multi-penetration measurements with in situ thermal conductivity, or deep sea drilling thermal gradients backed up by surface surveys. The 9 data points that result from this selection process have been plotted on a depth versus heat flow graph and compared to published thermal models of lithosphere. When considered without regard to age, all the points fall at greater depths than predicted by the ‘plate’ models with constant temperature lower boundaries, and remarkably close to boundary-layer cooling with parameters determined from the pre-80 Ma depth and heat flow history of the ocean floor. They are differentiated by their heat flows not much by their depths and the order they plot in along the heat flow axis is random with respect to crustal age. Modeling of discrete reheating events shows that near boundary layer conditions are re-established after about 40 Myr, but corresponding to a younger-than-real age. The data therefore favor discrete reheating events rather than a continuously hot basal boundary, as implicitly assumed by the plate model. Lithospheric reheating appears to start only on ocean floor > 100 Ma. The data alone cannot discriminate between a few discrete reheating events due to convective peel-off at the base of the lithosphere or one or more catastrophic events. However, the distribution of points from the Blake-Bahama basin is more consistent with distal reheating associated with the Bermuda hotspot than local convective peel-off." @default.
• W2055607114 created "2016-06-24" @default.
• W2055607114 creator A5032625754 @default.
• W2055607114 creator A5060264799 @default.
• W2055607114 creator A5062707313 @default.
• W2055607114 date "1996-03-01" @default.
• W2055607114 modified "2023-09-27" @default.
• W2055607114 title "Reheating of old oceanic lithosphere: Deductions from observations" @default.
• W2055607114 cites W1966289861 @default.
• W2055607114 cites W1967371674 @default.
• W2055607114 cites W1968028981 @default.
• W2055607114 cites W1973316520 @default.
• W2055607114 cites W1976052080 @default.
• W2055607114 cites W1977164751 @default.
• W2055607114 cites W1990740187 @default.
• W2055607114 cites W1990814837 @default.
• W2055607114 cites W1992891991 @default.
• W2055607114 cites W2007657452 @default.
• W2055607114 cites W2019991336 @default.
• W2055607114 cites W2020175339 @default.
• W2055607114 cites W2022648729 @default.
• W2055607114 cites W2025244602 @default.
• W2055607114 cites W2027765443 @default.
• W2055607114 cites W2033672857 @default.
• W2055607114 cites W2034616078 @default.
• W2055607114 cites W2034803972 @default.
• W2055607114 cites W2041868589 @default.
• W2055607114 cites W2054570249 @default.
• W2055607114 cites W2057620568 @default.
• W2055607114 cites W2070900495 @default.
• W2055607114 cites W2076314280 @default.
• W2055607114 cites W2077584717 @default.
• W2055607114 cites W2085845463 @default.
• W2055607114 cites W2096979079 @default.
• W2055607114 cites W2102234201 @default.
• W2055607114 cites W2114660893 @default.
• W2055607114 cites W2129426845 @default.
• W2055607114 cites W2131550905 @default.
• W2055607114 cites W2137911923 @default.
• W2055607114 cites W2147260309 @default.
• W2055607114 cites W2148437622 @default.
• W2055607114 cites W2150878580 @default.
• W2055607114 cites W2151625657 @default.
• W2055607114 cites W2153846210 @default.
• W2055607114 cites W2158555645 @default.
• W2055607114 cites W2164242909 @default.
• W2055607114 cites W2164827694 @default.
• W2055607114 cites W2500332345 @default.
• W2055607114 doi "https://doi.org/10.1016/0012-821x(96)00010-6" @default.
• W2055607114 hasPublicationYear "1996" @default.
• W2055607114 type Work @default.
• W2055607114 sameAs 2055607114 @default.
• W2055607114 citedByCount "42" @default.
• W2055607114 countsByYear W20556071142013 @default.
• W2055607114 countsByYear W20556071142014 @default.
• W2055607114 countsByYear W20556071142015 @default.
• W2055607114 countsByYear W20556071142017 @default.
• W2055607114 countsByYear W20556071142018 @default.
• W2055607114 countsByYear W20556071142019 @default.
• W2055607114 countsByYear W20556071142020 @default.
• W2055607114 countsByYear W20556071142021 @default.
• W2055607114 countsByYear W20556071142022 @default.
• W2055607114 crossrefType "journal-article" @default.
• W2055607114 hasAuthorship W2055607114A5032625754 @default.
• W2055607114 hasAuthorship W2055607114A5060264799 @default.
• W2055607114 hasAuthorship W2055607114A5062707313 @default.
• W2055607114 hasConcept C109007969 @default.
• W2055607114 hasConcept C111603439 @default.
• W2055607114 hasConcept C114793014 @default.
• W2055607114 hasConcept C117485682 @default.
• W2055607114 hasConcept C121332964 @default.
• W2055607114 hasConcept C127313418 @default.
• W2055607114 hasConcept C127413603 @default.
• W2055607114 hasConcept C142047668 @default.
• W2055607114 hasConcept C153294291 @default.
• W2055607114 hasConcept C165205528 @default.
• W2055607114 hasConcept C16942324 @default.
• W2055607114 hasConcept C20364790 @default.
• W2055607114 hasConcept C204530211 @default.
• W2055607114 hasConcept C25197100 @default.
• W2055607114 hasConcept C2985596519 @default.
• W2055607114 hasConcept C57879066 @default.
• W2055607114 hasConcept C5900021 @default.
• W2055607114 hasConcept C67236022 @default.
• W2055607114 hasConcept C77928131 @default.
• W2055607114 hasConcept C78519656 @default.
• W2055607114 hasConcept C8058405 @default.
• W2055607114 hasConcept C97346530 @default.
• W2055607114 hasConcept C97355855 @default.
• W2055607114 hasConceptScore W2055607114C109007969 @default.
• W2055607114 hasConceptScore W2055607114C111603439 @default.
• W2055607114 hasConceptScore W2055607114C114793014 @default.
• W2055607114 hasConceptScore W2055607114C117485682 @default.
• W2055607114 hasConceptScore W2055607114C121332964 @default.
• W2055607114 hasConceptScore W2055607114C127313418 @default.
• W2055607114 hasConceptScore W2055607114C127413603 @default.
• W2055607114 hasConceptScore W2055607114C142047668 @default.
• W2055607114 hasConceptScore W2055607114C153294291 @default.

• next