FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2103510367> ?p ?o ?g. }

• W2103510367 endingPage "1149" @default.
• W2103510367 startingPage "1131" @default.
• W2103510367 abstract "The crustal structure of central Iceland is modelled using data from a 310 km long refraction profile shot during summer 1995. The profile traversed Iceland from the Skagi Peninsula on the north coast (surface rocks of age 8.5–0.8 Myr) to the southeast coast (surface rocks of age 8.5–3.3 Myr), crossing central Iceland (surface rocks of age 3.3–0 Myr) over the glacier Vatnajökull, below which the locus of the Iceland mantle plume is currently centred. The crustal thickness is 25 km at the north end of the profile, increasing to 38–40 km beneath southern central Iceland. The upper crust is characterized by seismic P-wave velocities from 3.2 to approximately 6.4 km s−1. At the extreme ends of the profile, the upper crust can be modelled by a two-layered structure, within which seismic velocity increases with depth, with a total thickness of 5–6 km. The central highlands of Iceland have a single unit of upper crust, with seismic velocity increasing continuously with depth to almost 10 km below the surface. Below the central volcanoes of northern Vatnajökull, the upper crust is only 3 km thick. The lower-crustal velocity structure is determined from rays that turn at a maximum depth of 24 km below central Iceland, where the seismic velocity is 7.2 km s−1. Below 24 km depth there are no first-arriving turning rays. The Moho is defined by P-and S-wave reflections observed from the shots at the extreme ends of the profile.P- to S-wave velocity ratios give a Poisson's:of 0.26 in the upper crust and 0.27 in the lower crust, indicating that, even directly above the centre of the mantle plume, the crust is well below the solidus temperature." @default.
• W2103510367 created "2016-06-24" @default.
• W2103510367 creator A5014652050 @default.
• W2103510367 creator A5021139994 @default.
• W2103510367 creator A5059097383 @default.
• W2103510367 creator A5080796115 @default.
• W2103510367 date "1998-12-01" @default.
• W2103510367 modified "2023-10-05" @default.
• W2103510367 title "Crustal structure above the Iceland mantle plume imaged by the ICEMELT refraction profile" @default.
• W2103510367 cites W1981820175 @default.
• W2103510367 cites W1992891991 @default.
• W2103510367 cites W1996186259 @default.
• W2103510367 cites W1997436175 @default.
• W2103510367 cites W1999899533 @default.
• W2103510367 cites W2006745337 @default.
• W2103510367 cites W2009114652 @default.
• W2103510367 cites W2010441507 @default.
• W2103510367 cites W2014220172 @default.
• W2103510367 cites W2051208759 @default.
• W2103510367 cites W2052728319 @default.
• W2103510367 cites W2055566826 @default.
• W2103510367 cites W2058884294 @default.
• W2103510367 cites W2060087216 @default.
• W2103510367 cites W2067349192 @default.
• W2103510367 cites W2072646360 @default.
• W2103510367 cites W2077584717 @default.
• W2103510367 cites W2083142278 @default.
• W2103510367 cites W2085173581 @default.
• W2103510367 cites W2087840204 @default.
• W2103510367 cites W2089537803 @default.
• W2103510367 cites W2099044166 @default.
• W2103510367 cites W2101538421 @default.
• W2103510367 cites W2114964712 @default.
• W2103510367 cites W2122036745 @default.
• W2103510367 cites W2130833734 @default.
• W2103510367 cites W2145594692 @default.
• W2103510367 cites W2153511421 @default.
• W2103510367 cites W2159506096 @default.
• W2103510367 cites W2161489274 @default.
• W2103510367 cites W2167078496 @default.
• W2103510367 cites W2168959606 @default.
• W2103510367 cites W2289488404 @default.
• W2103510367 cites W2301587032 @default.
• W2103510367 cites W4251374604 @default.
• W2103510367 cites W4322391631 @default.
• W2103510367 cites W4322391662 @default.
• W2103510367 doi "https://doi.org/10.1046/j.1365-246x.1998.00701.x" @default.
• W2103510367 hasPublicationYear "1998" @default.
• W2103510367 type Work @default.
• W2103510367 sameAs 2103510367 @default.
• W2103510367 citedByCount "131" @default.
• W2103510367 countsByYear W21035103672012 @default.
• W2103510367 countsByYear W21035103672013 @default.
• W2103510367 countsByYear W21035103672014 @default.
• W2103510367 countsByYear W21035103672015 @default.
• W2103510367 countsByYear W21035103672016 @default.
• W2103510367 countsByYear W21035103672017 @default.
• W2103510367 countsByYear W21035103672018 @default.
• W2103510367 countsByYear W21035103672019 @default.
• W2103510367 countsByYear W21035103672020 @default.
• W2103510367 countsByYear W21035103672021 @default.
• W2103510367 countsByYear W21035103672022 @default.
• W2103510367 countsByYear W21035103672023 @default.
• W2103510367 crossrefType "journal-article" @default.
• W2103510367 hasAuthorship W2103510367A5014652050 @default.
• W2103510367 hasAuthorship W2103510367A5021139994 @default.
• W2103510367 hasAuthorship W2103510367A5059097383 @default.
• W2103510367 hasAuthorship W2103510367A5080796115 @default.
• W2103510367 hasBestOaLocation W21035103671 @default.
• W2103510367 hasConcept C111461898 @default.
• W2103510367 hasConcept C120806208 @default.
• W2103510367 hasConcept C127313418 @default.
• W2103510367 hasConcept C141646446 @default.
• W2103510367 hasConcept C165205528 @default.
• W2103510367 hasConcept C2776698055 @default.
• W2103510367 hasConcept C8058405 @default.
• W2103510367 hasConceptScore W2103510367C111461898 @default.
• W2103510367 hasConceptScore W2103510367C120806208 @default.
• W2103510367 hasConceptScore W2103510367C127313418 @default.
• W2103510367 hasConceptScore W2103510367C141646446 @default.
• W2103510367 hasConceptScore W2103510367C165205528 @default.
• W2103510367 hasConceptScore W2103510367C2776698055 @default.
• W2103510367 hasConceptScore W2103510367C8058405 @default.
• W2103510367 hasIssue "3" @default.
• W2103510367 hasLocation W21035103671 @default.
• W2103510367 hasLocation W21035103672 @default.
• W2103510367 hasOpenAccess W2103510367 @default.
• W2103510367 hasPrimaryLocation W21035103671 @default.
• W2103510367 hasRelatedWork W1999697500 @default.
• W2103510367 hasRelatedWork W2032127348 @default.
• W2103510367 hasRelatedWork W2048372491 @default.
• W2103510367 hasRelatedWork W2089045238 @default.
• W2103510367 hasRelatedWork W2147270527 @default.
• W2103510367 hasRelatedWork W2171935214 @default.
• W2103510367 hasRelatedWork W2271740537 @default.
• W2103510367 hasRelatedWork W2613589034 @default.
• W2103510367 hasRelatedWork W3033545842 @default.
• W2103510367 hasRelatedWork W4232514517 @default.

• next