Matches in SemOpenAlex for { <https://semopenalex.org/work/W2338577013> ?p ?o ?g. }
Showing items 1 to 73 of
73
with 100 items per page.
- W2338577013 abstract "The SCANLIPS 3D experiment deployed 20 ESP seismometers in northern central Norway and Sweden between June 2013 and September 2014 to investigate the cause of the high topography which dominates Norway and process of topographic uplift. 97% data recovery was achieved. Data quality showed the ESP instruments performed well in comparison to 3T instruments previously deployed in Scandinavia. Over 400 receiver functions were calculated from teleseismic events recorded across the array. Inverse modelling and h-κ stacking of these receiver functions show there is no linear crustal root supporting the present day high topography. A region of thick crust which correlates with a negative residual isostatic gravity anomaly appears to confirm that locally the crust is overcompensated. Comparisons between the surface geology and variations in crustal structure and Moho sharpness suggest that the Caledonian orogeny may have reworked the Proterozoic basement, removing a high velocity lower crustal layer. Background: The SCANLIPS3D experiment builds on existing work conducted in Norway and Sweden (SCANLIPS and SCANLIPS2) to investigate the possible cause of the geologically recent (Miocene) uplift which has affected Scandinavia (Fig. 1). The Scandes mountains show high topography in the south (described by Svenningsen et al. 2007) relatively low topography in central Norway and Sweden (England and Ebbing 2012) and high topography in the North (Ebbing et al. 2012) which it is believed was created by the same regional uplift event. Because of the relatively short wavelength variations in topography, it is suspected that the variations in present day relief are Fig. 1. Topographic map of Scandinavia. SCANLIPS3D stations shown as white squares. Red squares are SCANLIPS stations and SCANLIPS2 stations are shown in green. Thin blue lines are existing refraction profiles. Other symbols are broadband seismic stations deployed as part of the CENMOVE experiment. NERC Geophysical Equipment Facility View more reports on our website at http://gef.nerc.ac.uk/reports.php" @default.
- W2338577013 created "2016-06-24" @default.
- W2338577013 creator A5026210800 @default.
- W2338577013 creator A5026878453 @default.
- W2338577013 creator A5030830880 @default.
- W2338577013 date "2015-01-01" @default.
- W2338577013 modified "2023-09-26" @default.
- W2338577013 title "SCANLIPS3D - SCANdinavian LIthosphere P and S wave experiment 3 D" @default.
- W2338577013 cites W1997204737 @default.
- W2338577013 cites W2155484979 @default.
- W2338577013 hasPublicationYear "2015" @default.
- W2338577013 type Work @default.
- W2338577013 sameAs 2338577013 @default.
- W2338577013 citedByCount "0" @default.
- W2338577013 crossrefType "journal-article" @default.
- W2338577013 hasAuthorship W2338577013A5026210800 @default.
- W2338577013 hasAuthorship W2338577013A5026878453 @default.
- W2338577013 hasAuthorship W2338577013A5030830880 @default.
- W2338577013 hasConcept C119217923 @default.
- W2338577013 hasConcept C122792734 @default.
- W2338577013 hasConcept C127313418 @default.
- W2338577013 hasConcept C127413603 @default.
- W2338577013 hasConcept C13280743 @default.
- W2338577013 hasConcept C147176958 @default.
- W2338577013 hasConcept C151730666 @default.
- W2338577013 hasConcept C165205528 @default.
- W2338577013 hasConcept C16942324 @default.
- W2338577013 hasConcept C2776698055 @default.
- W2338577013 hasConcept C2777241186 @default.
- W2338577013 hasConcept C2781297371 @default.
- W2338577013 hasConcept C77928131 @default.
- W2338577013 hasConcept C93033518 @default.
- W2338577013 hasConceptScore W2338577013C119217923 @default.
- W2338577013 hasConceptScore W2338577013C122792734 @default.
- W2338577013 hasConceptScore W2338577013C127313418 @default.
- W2338577013 hasConceptScore W2338577013C127413603 @default.
- W2338577013 hasConceptScore W2338577013C13280743 @default.
- W2338577013 hasConceptScore W2338577013C147176958 @default.
- W2338577013 hasConceptScore W2338577013C151730666 @default.
- W2338577013 hasConceptScore W2338577013C165205528 @default.
- W2338577013 hasConceptScore W2338577013C16942324 @default.
- W2338577013 hasConceptScore W2338577013C2776698055 @default.
- W2338577013 hasConceptScore W2338577013C2777241186 @default.
- W2338577013 hasConceptScore W2338577013C2781297371 @default.
- W2338577013 hasConceptScore W2338577013C77928131 @default.
- W2338577013 hasConceptScore W2338577013C93033518 @default.
- W2338577013 hasLocation W23385770131 @default.
- W2338577013 hasOpenAccess W2338577013 @default.
- W2338577013 hasPrimaryLocation W23385770131 @default.
- W2338577013 hasRelatedWork W1888473130 @default.
- W2338577013 hasRelatedWork W2012390116 @default.
- W2338577013 hasRelatedWork W2038427246 @default.
- W2338577013 hasRelatedWork W2040056822 @default.
- W2338577013 hasRelatedWork W2055878775 @default.
- W2338577013 hasRelatedWork W2081642393 @default.
- W2338577013 hasRelatedWork W2099730240 @default.
- W2338577013 hasRelatedWork W2120685923 @default.
- W2338577013 hasRelatedWork W2141906016 @default.
- W2338577013 hasRelatedWork W2164309078 @default.
- W2338577013 hasRelatedWork W2164779276 @default.
- W2338577013 hasRelatedWork W2292075498 @default.
- W2338577013 hasRelatedWork W2512079528 @default.
- W2338577013 hasRelatedWork W254385536 @default.
- W2338577013 hasRelatedWork W2905420532 @default.
- W2338577013 hasRelatedWork W2986659021 @default.
- W2338577013 hasRelatedWork W3003753015 @default.
- W2338577013 hasRelatedWork W3109636541 @default.
- W2338577013 hasRelatedWork W359410522 @default.
- W2338577013 hasRelatedWork W2320097323 @default.
- W2338577013 isParatext "false" @default.
- W2338577013 isRetracted "false" @default.
- W2338577013 magId "2338577013" @default.
- W2338577013 workType "article" @default.