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dc.contributor.authorBeka, Thomas Ibsa
dc.contributor.authorSmirnov, Maxim
dc.contributor.authorBergh, Steffen G
dc.contributor.authorBirkelund, Yngve
dc.date.accessioned2016-03-04T12:16:27Z
dc.date.available2016-03-04T12:16:27Z
dc.date.issued2015-12-17
dc.description.abstractMagnetotelluric data, collected from 30 stations on Spitsbergen as part of a reconnaissance geothermal resource assessment along a profile with 0.53-km spacing in 0.0031000-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 (B100 Vm) Paleozoic Mesozoic sedimentary sequence, varying laterally in thickness (24 km), obstructed by a gently dipping PermianCarboniferous succession (1000 Vm) 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 PaleozoicMesozoic successions, an uplifted pre-Devonian shallow basement (3000 Vm) is revealed. We estimated a thin lithosphere, in the range of ca. 55100 km thick, that could explain the area’s elevated surface heat flow (ca. 6090 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. Human seten_US
dc.identifier.citationPolar Research 2015, 34( 26766)en_US
dc.identifier.cristinIDFRIDAID 1247857
dc.identifier.doi10.3402/polar.v34.26766
dc.identifier.issn1751-8369
dc.identifier.urihttps://hdl.handle.net/10037/8696
dc.identifier.urnURN:NBN:no-uit_munin_8268
dc.language.isoengen_US
dc.publisherCo-Action Publishingen_US
dc.relation.urihttp://www.polarresearch.net/index.php/polar/article/view/26766en_US
dc.rights.accessRightsopenAccess
dc.subjectMagnetotelluricsen_US
dc.subject2D modellingen_US
dc.subjectlithosphere architectureen_US
dc.subjectgeothermaen_US
dc.subjectSvalbarden_US
dc.subjectVDP::Matematikk og Naturvitenskap: 400::Geofag: 450en_US
dc.subjectVDP::Mathematics and natural science: 400::Geosciences: 450en_US
dc.titleThe First Magnetotelluric Image of the Lithospheric-Scale Geological Architecture in Central Svalbard, Arctic Norwayen_US
dc.typeJournal articleen_US
dc.typeTidsskriftartikkelen_US
dc.typePeer revieweden_US


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