FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2060952854> ?p ?o ?g. }

• W2060952854 endingPage "1148" @default.
• W2060952854 startingPage "1133" @default.
• W2060952854 abstract "It is likely that the structure of a volcanic edifice can be significantly modified by deformation caused by large, shallow intrusions. Such deformation may interact with that caused by volcano loading. We explore such intrusion-related and loading-related deformation with field evidence and analogue models. To do this we have chosen the eroded Palaeogene Mull volcano (Scotland) that had a major edifice, has well exposed intrusions and significant deformation. There are thin Mesozoic sedimentary rocks forming ductile layers below the volcano, but their thickness is insufficient to allow the gravitational spreading of the volcanic edifice, especially when considering that a thick lava pile covers them. Thus intrusive push may have been the driving force for deformation. The Mull activity migrated toward the northwest, forming three successive intrusive complexes (Centres 1, 2 and 3). Our detailed fieldwork reveals that deformation due to these was accommodated on three levels; along thrust planes in lava sequences, along a décollement located in a thin clay-rich sediment succession and in basement schists. A relative chronology has been established between different groups of structures using dyke and sill cross-cutting relationships. Centre 1 is surrounded by a fold and thrust belt leading to radial expansion. In contrast, Centre 2 and 3 are connected to thrusts located to the south and east, bounded by strike-slip faults, leading to expansion to the southeast. The migration of centres and the directed sliding of the edifice may be related to the presence to the southeast of low-resistance Dalradian basement that failed significantly during growth of Centres 2 and 3. To study the observed relationships we have carried out scaled analogue models. Models are made with fine powder intruded by a viscous magma analogue. The models show an intimate relationship between intrusion growth, uplift of the volcano and subsequent flank sliding. The structures produced can be compared with Mull and suggest that the Centre 1 thrust belt probably formed following edifice gravitational sliding as a consequence of the uplift associated with Centre 1 formation. Centre 2 and 3 are responsible for the sector sliding of the edifice flank toward the southeast as the magmatic complex became more asymmetric. The features observed at Mull and in the models are similar to those seen on active volcanoes, such as Etna, providing a structural framework for their deformation and evolution." @default.
• W2060952854 created "2016-06-24" @default.
• W2060952854 creator A5017166062 @default.
• W2060952854 creator A5044906448 @default.
• W2060952854 date "2009-05-28" @default.
• W2060952854 modified "2023-09-26" @default.
• W2060952854 title "Edifice and substrata deformation induced by intrusive complexes and gravitational loading in the Mull volcano (Scotland)" @default.
• W2060952854 cites W1624813937 @default.
• W2060952854 cites W1982593316 @default.
• W2060952854 cites W1983363847 @default.
• W2060952854 cites W1986991049 @default.
• W2060952854 cites W2007940282 @default.
• W2060952854 cites W2021644533 @default.
• W2060952854 cites W2037478172 @default.
• W2060952854 cites W2039202144 @default.
• W2060952854 cites W2047891230 @default.
• W2060952854 cites W2056566505 @default.
• W2060952854 cites W2059121530 @default.
• W2060952854 cites W2084931712 @default.
• W2060952854 cites W2086057813 @default.
• W2060952854 cites W2093446310 @default.
• W2060952854 cites W2099771249 @default.
• W2060952854 cites W2101342695 @default.
• W2060952854 cites W2107259349 @default.
• W2060952854 cites W2111710951 @default.
• W2060952854 cites W2152171637 @default.
• W2060952854 cites W2153846210 @default.
• W2060952854 cites W2164796906 @default.
• W2060952854 cites W2167669185 @default.
• W2060952854 cites W2317335583 @default.
• W2060952854 doi "https://doi.org/10.1007/s00445-009-0295-5" @default.
• W2060952854 hasPublicationYear "2009" @default.
• W2060952854 type Work @default.
• W2060952854 sameAs 2060952854 @default.
• W2060952854 citedByCount "24" @default.
• W2060952854 countsByYear W20609528542012 @default.
• W2060952854 countsByYear W20609528542014 @default.
• W2060952854 countsByYear W20609528542015 @default.
• W2060952854 countsByYear W20609528542017 @default.
• W2060952854 countsByYear W20609528542018 @default.
• W2060952854 countsByYear W20609528542020 @default.
• W2060952854 countsByYear W20609528542021 @default.
• W2060952854 countsByYear W20609528542023 @default.
• W2060952854 crossrefType "journal-article" @default.
• W2060952854 hasAuthorship W2060952854A5017166062 @default.
• W2060952854 hasAuthorship W2060952854A5044906448 @default.
• W2060952854 hasBestOaLocation W20609528541 @default.
• W2060952854 hasConcept C110041135 @default.
• W2060952854 hasConcept C113754120 @default.
• W2060952854 hasConcept C120806208 @default.
• W2060952854 hasConcept C127313418 @default.
• W2060952854 hasConcept C165205528 @default.
• W2060952854 hasConcept C17409809 @default.
• W2060952854 hasConcept C175551986 @default.
• W2060952854 hasConcept C40201923 @default.
• W2060952854 hasConcept C52543455 @default.
• W2060952854 hasConcept C5900021 @default.
• W2060952854 hasConcept C6494504 @default.
• W2060952854 hasConcept C80781247 @default.
• W2060952854 hasConceptScore W2060952854C110041135 @default.
• W2060952854 hasConceptScore W2060952854C113754120 @default.
• W2060952854 hasConceptScore W2060952854C120806208 @default.
• W2060952854 hasConceptScore W2060952854C127313418 @default.
• W2060952854 hasConceptScore W2060952854C165205528 @default.
• W2060952854 hasConceptScore W2060952854C17409809 @default.
• W2060952854 hasConceptScore W2060952854C175551986 @default.
• W2060952854 hasConceptScore W2060952854C40201923 @default.
• W2060952854 hasConceptScore W2060952854C52543455 @default.
• W2060952854 hasConceptScore W2060952854C5900021 @default.
• W2060952854 hasConceptScore W2060952854C6494504 @default.
• W2060952854 hasConceptScore W2060952854C80781247 @default.
• W2060952854 hasIssue "10" @default.
• W2060952854 hasLocation W20609528541 @default.
• W2060952854 hasOpenAccess W2060952854 @default.
• W2060952854 hasPrimaryLocation W20609528541 @default.
• W2060952854 hasRelatedWork W1966570635 @default.
• W2060952854 hasRelatedWork W2012046692 @default.
• W2060952854 hasRelatedWork W2019718787 @default.
• W2060952854 hasRelatedWork W2037725488 @default.
• W2060952854 hasRelatedWork W2070192581 @default.
• W2060952854 hasRelatedWork W2364766047 @default.
• W2060952854 hasRelatedWork W2390287242 @default.
• W2060952854 hasRelatedWork W2916229122 @default.
• W2060952854 hasRelatedWork W3123071480 @default.
• W2060952854 hasRelatedWork W533705 @default.
• W2060952854 hasVolume "71" @default.
• W2060952854 isParatext "false" @default.
• W2060952854 isRetracted "false" @default.
• W2060952854 magId "2060952854" @default.
• W2060952854 workType "article" @default.