FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2081796369> ?p ?o ?g. }

• W2081796369 endingPage "6418" @default.
• W2081796369 startingPage "6403" @default.
• W2081796369 abstract "One of the principal arguments for large stress differences in the lithosphere comes from the modeling of the deflection of the ocean lithosphere under seamount loads. Most published models indicate maximum stress differences of 2–3 kbar per kilometer of deflection, and maximum values approach 10 kbar. Geophysical support for the elastic plate theory comes mainly from gravity, which requires a broad negative anomaly on the flanks of the actual seamount, although these anomalies are not very sensitive to the density structure of the crust or to the density of the sediment fill‐in or the extent of this fill‐in. The stress in the plate, however, is sensitive to these parameters, and in consequence, gravity is not a reliable indicator of the stress state. The lithospheric flexure model has been examined in some detail to evaluate this stress dependence on crustal densities and rheology. The approximations inherent in the linear theory have also been investigated. The main conclusions are that the stress differences can be significantly reduced (1) by adopting a lower density for the sediment fill‐in than the usual 2.8 g cm −3 , (2) by introducing a depth‐dependent nonelastic rheology, and (3) by introducing large‐deflection theory for the larger loads. For large loads, such as Oahu Island discussed by Watts (1978), the maximum stress under the load can be reduced to about 2 kbar or less near the upper surface of the plate, and the maximum stress differences σ rr ‐ σ zz need not exceed 1 kbar. The introduction of the nonelastic rheology results in a stress, temperature, and load duration dependence of the ‘apparent’ flexural rigidity; large loads, loads of long duration, or loads on a high‐temperature lithosphere all result in a thinner apparent plate thickness than small loads, loads of short duration, or loads on a cool lithosphere, all other factors being equal." @default.
• W2081796369 created "2016-06-24" @default.
• W2081796369 creator A5049983897 @default.
• W2081796369 creator A5084891677 @default.
• W2081796369 date "1980-11-10" @default.
• W2081796369 modified "2023-09-27" @default.
• W2081796369 title "Seamount loading and stress in the ocean lithosphere" @default.
• W2081796369 cites W1547300557 @default.
• W2081796369 cites W1552311529 @default.
• W2081796369 cites W1641908062 @default.
• W2081796369 cites W1966959041 @default.
• W2081796369 cites W1968087724 @default.
• W2081796369 cites W1971436896 @default.
• W2081796369 cites W1989284742 @default.
• W2081796369 cites W2001974610 @default.
• W2081796369 cites W2005789596 @default.
• W2081796369 cites W2029334027 @default.
• W2081796369 cites W2036429060 @default.
• W2081796369 cites W2047758248 @default.
• W2081796369 cites W2049890027 @default.
• W2081796369 cites W2055370415 @default.
• W2081796369 cites W2059983526 @default.
• W2081796369 cites W2060419201 @default.
• W2081796369 cites W2060745044 @default.
• W2081796369 cites W2106781958 @default.
• W2081796369 cites W2129488625 @default.
• W2081796369 cites W2136062812 @default.
• W2081796369 cites W2148680942 @default.
• W2081796369 cites W2160455456 @default.
• W2081796369 cites W2226710728 @default.
• W2081796369 cites W3172485659 @default.
• W2081796369 cites W4255325196 @default.
• W2081796369 doi "https://doi.org/10.1029/jb085ib11p06403" @default.
• W2081796369 hasPublicationYear "1980" @default.
• W2081796369 type Work @default.
• W2081796369 sameAs 2081796369 @default.
• W2081796369 citedByCount "95" @default.
• W2081796369 countsByYear W20817963692012 @default.
• W2081796369 countsByYear W20817963692013 @default.
• W2081796369 countsByYear W20817963692014 @default.
• W2081796369 countsByYear W20817963692015 @default.
• W2081796369 countsByYear W20817963692016 @default.
• W2081796369 countsByYear W20817963692017 @default.
• W2081796369 countsByYear W20817963692019 @default.
• W2081796369 countsByYear W20817963692020 @default.
• W2081796369 countsByYear W20817963692021 @default.
• W2081796369 countsByYear W20817963692022 @default.
• W2081796369 crossrefType "journal-article" @default.
• W2081796369 hasAuthorship W2081796369A5049983897 @default.
• W2081796369 hasAuthorship W2081796369A5084891677 @default.
• W2081796369 hasConcept C111368507 @default.
• W2081796369 hasConcept C120665830 @default.
• W2081796369 hasConcept C121332964 @default.
• W2081796369 hasConcept C127313418 @default.
• W2081796369 hasConcept C135559958 @default.
• W2081796369 hasConcept C138885662 @default.
• W2081796369 hasConcept C151730666 @default.
• W2081796369 hasConcept C159985019 @default.
• W2081796369 hasConcept C165205528 @default.
• W2081796369 hasConcept C16942324 @default.
• W2081796369 hasConcept C192562407 @default.
• W2081796369 hasConcept C200990466 @default.
• W2081796369 hasConcept C21036866 @default.
• W2081796369 hasConcept C2776364302 @default.
• W2081796369 hasConcept C2776698055 @default.
• W2081796369 hasConcept C2781355719 @default.
• W2081796369 hasConcept C41895202 @default.
• W2081796369 hasConcept C77928131 @default.
• W2081796369 hasConcept C8058405 @default.
• W2081796369 hasConcept C96342900 @default.
• W2081796369 hasConceptScore W2081796369C111368507 @default.
• W2081796369 hasConceptScore W2081796369C120665830 @default.
• W2081796369 hasConceptScore W2081796369C121332964 @default.
• W2081796369 hasConceptScore W2081796369C127313418 @default.
• W2081796369 hasConceptScore W2081796369C135559958 @default.
• W2081796369 hasConceptScore W2081796369C138885662 @default.
• W2081796369 hasConceptScore W2081796369C151730666 @default.
• W2081796369 hasConceptScore W2081796369C159985019 @default.
• W2081796369 hasConceptScore W2081796369C165205528 @default.
• W2081796369 hasConceptScore W2081796369C16942324 @default.
• W2081796369 hasConceptScore W2081796369C192562407 @default.
• W2081796369 hasConceptScore W2081796369C200990466 @default.
• W2081796369 hasConceptScore W2081796369C21036866 @default.
• W2081796369 hasConceptScore W2081796369C2776364302 @default.
• W2081796369 hasConceptScore W2081796369C2776698055 @default.
• W2081796369 hasConceptScore W2081796369C2781355719 @default.
• W2081796369 hasConceptScore W2081796369C41895202 @default.
• W2081796369 hasConceptScore W2081796369C77928131 @default.
• W2081796369 hasConceptScore W2081796369C8058405 @default.
• W2081796369 hasConceptScore W2081796369C96342900 @default.
• W2081796369 hasIssue "B11" @default.
• W2081796369 hasLocation W20817963691 @default.
• W2081796369 hasOpenAccess W2081796369 @default.
• W2081796369 hasPrimaryLocation W20817963691 @default.
• W2081796369 hasRelatedWork W1547300557 @default.
• W2081796369 hasRelatedWork W2002175295 @default.
• W2081796369 hasRelatedWork W2020899413 @default.
• W2081796369 hasRelatedWork W2336057781 @default.

• next