FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2208757650> ?p ?o ?g. }

• W2208757650 endingPage "26766" @default.
• W2208757650 startingPage "26766" @default.
• W2208757650 abstract "Magnetotelluric data, collected from 30 stations on Spitsbergen as part of a reconnaissance geothermal resource assessment along a profile with 0.5–3-km spacing in 0.003–1000-s period range, were used to develop a lithospheric-scale two-dimensional (2D) resistivity model, heretofore unavailable for the region. Inverting the determinant of the impedance tensor in 2D, we found the smoothest model fitting the data within a specified tolerance level. We justified the model by perturbing it, performing sensitivity analysis and re-running the inversion with a different algorithm and starting models. From our final model, we constructed a crustal-scale stratigraphic framework, using it to estimate the depth of major geological features and to locate structural deformations. The 2D resistivity model indicates a shallow low resistive (<100 Ωm) Paleozoic–Mesozoic sedimentary sequence, varying laterally in thickness (2–4 km), obstructed by a gently dipping Permian–Carboniferous succession (>1000 Ωm) east of the Billefjorden Fault Zone. Underneath, a (possibly Devonian) basin is imaged as a thick conductive anomaly stretching >15 km downwards. Beneath a deformed Paleozoic–Mesozoic successions, an uplifted pre-Devonian shallow basement (>3000 Ωm) is revealed. We estimated a thin lithosphere, in the range of ca. 55–100 km thick, that could explain the area’s elevated surface heat flow (ca. 60–90 mW/m2), consistent with the calculated depth of thermal lithosphere heat-base boundaries for a partially melting mantle. The model indicates a possible replenishment pathway of upward heat transport from the shallow convective mantle to the composite crustal conductive units. This is encouraging for low-enthalpy geothermal development.Keywords: Magnetotellurics; 2D modelling; lithosphere architecture; geothermal; Svalbard.(Published: 17 December 2015)Citation: Polar Research 2015, 34, 26766, http://dx.doi.org/10.3402/polar.v34.26766" @default.
• W2208757650 created "2016-06-24" @default.
• W2208757650 creator A5014763202 @default.
• W2208757650 creator A5024449269 @default.
• W2208757650 creator A5054100932 @default.
• W2208757650 creator A5060697411 @default.
• W2208757650 date "2015-01-01" @default.
• W2208757650 modified "2023-10-16" @default.
• W2208757650 title "The first magnetotelluric image of the lithospheric-scale geological architecture in central Svalbard, Arctic Norway" @default.
• W2208757650 cites W103455674 @default.
• W2208757650 cites W1967347187 @default.
• W2208757650 cites W1975551669 @default.
• W2208757650 cites W1983011160 @default.
• W2208757650 cites W1998092187 @default.
• W2208757650 cites W2013459156 @default.
• W2208757650 cites W2031195490 @default.
• W2208757650 cites W2035201317 @default.
• W2208757650 cites W2043285343 @default.
• W2208757650 cites W2048104607 @default.
• W2208757650 cites W2055242265 @default.
• W2208757650 cites W2061715959 @default.
• W2208757650 cites W2063349046 @default.
• W2208757650 cites W2072057519 @default.
• W2208757650 cites W2072179495 @default.
• W2208757650 cites W2073083908 @default.
• W2208757650 cites W2080334760 @default.
• W2208757650 cites W2084579489 @default.
• W2208757650 cites W2086496485 @default.
• W2208757650 cites W2086633317 @default.
• W2208757650 cites W2090072357 @default.
• W2208757650 cites W2096059159 @default.
• W2208757650 cites W2103709024 @default.
• W2208757650 cites W2108064160 @default.
• W2208757650 cites W2110535686 @default.
• W2208757650 cites W2119191748 @default.
• W2208757650 cites W2122170486 @default.
• W2208757650 cites W2127171935 @default.
• W2208757650 cites W2138251028 @default.
• W2208757650 cites W2157796583 @default.
• W2208757650 cites W2160180808 @default.
• W2208757650 cites W2160868630 @default.
• W2208757650 cites W2163063149 @default.
• W2208757650 cites W2166465211 @default.
• W2208757650 cites W4211215503 @default.
• W2208757650 cites W571871743 @default.
• W2208757650 doi "https://doi.org/10.3402/polar.v34.26766" @default.
• W2208757650 hasPublicationYear "2015" @default.
• W2208757650 type Work @default.
• W2208757650 sameAs 2208757650 @default.
• W2208757650 citedByCount "12" @default.
• W2208757650 countsByYear W22087576502016 @default.
• W2208757650 countsByYear W22087576502017 @default.
• W2208757650 countsByYear W22087576502018 @default.
• W2208757650 countsByYear W22087576502019 @default.
• W2208757650 countsByYear W22087576502020 @default.
• W2208757650 countsByYear W22087576502022 @default.
• W2208757650 countsByYear W22087576502023 @default.
• W2208757650 crossrefType "journal-article" @default.
• W2208757650 hasAuthorship W2208757650A5014763202 @default.
• W2208757650 hasAuthorship W2208757650A5024449269 @default.
• W2208757650 hasAuthorship W2208757650A5054100932 @default.
• W2208757650 hasAuthorship W2208757650A5060697411 @default.
• W2208757650 hasBestOaLocation W22087576501 @default.
• W2208757650 hasConcept C107832698 @default.
• W2208757650 hasConcept C111766609 @default.
• W2208757650 hasConcept C112313211 @default.
• W2208757650 hasConcept C114793014 @default.
• W2208757650 hasConcept C119599485 @default.
• W2208757650 hasConcept C122792734 @default.
• W2208757650 hasConcept C127313418 @default.
• W2208757650 hasConcept C127413603 @default.
• W2208757650 hasConcept C13106087 @default.
• W2208757650 hasConcept C150999391 @default.
• W2208757650 hasConcept C151730666 @default.
• W2208757650 hasConcept C162973429 @default.
• W2208757650 hasConcept C165205528 @default.
• W2208757650 hasConcept C16942324 @default.
• W2208757650 hasConcept C2776698055 @default.
• W2208757650 hasConcept C5900021 @default.
• W2208757650 hasConcept C6494504 @default.
• W2208757650 hasConcept C67236022 @default.
• W2208757650 hasConcept C69990965 @default.
• W2208757650 hasConcept C77928131 @default.
• W2208757650 hasConcept C8058405 @default.
• W2208757650 hasConceptScore W2208757650C107832698 @default.
• W2208757650 hasConceptScore W2208757650C111766609 @default.
• W2208757650 hasConceptScore W2208757650C112313211 @default.
• W2208757650 hasConceptScore W2208757650C114793014 @default.
• W2208757650 hasConceptScore W2208757650C119599485 @default.
• W2208757650 hasConceptScore W2208757650C122792734 @default.
• W2208757650 hasConceptScore W2208757650C127313418 @default.
• W2208757650 hasConceptScore W2208757650C127413603 @default.
• W2208757650 hasConceptScore W2208757650C13106087 @default.
• W2208757650 hasConceptScore W2208757650C150999391 @default.
• W2208757650 hasConceptScore W2208757650C151730666 @default.
• W2208757650 hasConceptScore W2208757650C162973429 @default.
• W2208757650 hasConceptScore W2208757650C165205528 @default.
• W2208757650 hasConceptScore W2208757650C16942324 @default.

• next