Multiscale interpretation and scaling analysis of the censored brittle structural framework within the crystalline bedrock of Southern Finland

dc.contributor.authorNordbäck Nicklas
dc.contributor.authorOvaskainen Nikolas
dc.contributor.authorMarkovaara-Koivisto Mira
dc.contributor.authorSkyttä Pietari
dc.contributor.authorOjala Antti E.K.
dc.contributor.authorEngström Jon
dc.contributor.authorNixon Casey
dc.contributor.organizationfi=geologia|en=Geology |
dc.contributor.organization-code1.2.246.10.2458963.20.72020864681
dc.contributor.organization-code2606902
dc.converis.publication-id180490283
dc.converis.urlhttps://research.utu.fi/converis/portal/Publication/180490283
dc.date.accessioned2025-08-27T21:30:17Z
dc.date.available2025-08-27T21:30:17Z
dc.description.abstract<p>Fracture studies commonly lack data for the length range between 10 m to 1 km. For this reason, scaling laws are required to extrapolate fracture properties, for example in discrete fracture network models. This study focused on analysis and correlation of topology, orientation and length distribution of multiscale fracture datasets to assess their scalability. The used datasets comprise UAV-derived photogrammetric models from natural outcrops and lineaments mapped using airborne LiDAR, bathymetry and aerogeophysical data, in several contrasting scales and resolutions. This study highlights challenges in acquiring uncensored and coherent brittle structural datasets from source data characterized by a large span of resolutions between the remote sensing datasets and models of the fractured outcrop. In specific, collected data was found to be potentially biased and affected by uncertainties related to both the censoring by sedimentary cover and the scale of observation. Our results revealed differences between lineament and outcrop fracture orientations, as well as difficulties in assessing topological parameters from lineament datasets. The 1:200000 resolution was found best suited to the mapping of lineament length and resulted in a length distribution power law exponent of -1.92. For outcrop fractures that are less than 2 m long, the lognormal length distribution provided the only good fit to our data, while the longer outcrop fractures fitted relatively well with a power law exponent of -2.26.</p>
dc.format.pagerange32
dc.format.pagerange5
dc.identifier.eissn1799-4632
dc.identifier.jour-issn0367-5211
dc.identifier.olddbid200519
dc.identifier.oldhandle10024/183546
dc.identifier.urihttps://www.utupub.fi/handle/11111/46806
dc.identifier.urlhttps://doi.org/10.17741/bgsf/95.1.001
dc.identifier.urnURN:NBN:fi-fe2025082785035
dc.language.isoen
dc.okm.affiliatedauthorNordbäck, Nicklas
dc.okm.affiliatedauthorOvaskainen, Nikolas
dc.okm.affiliatedauthorSkyttä, Pietari
dc.okm.affiliatedauthorOjala, Antti
dc.okm.discipline1171 Geosciencesen_GB
dc.okm.discipline1171 Geotieteetfi_FI
dc.okm.internationalcopublicationinternational co-publication
dc.okm.internationalityDomestic publication
dc.okm.typeA1 ScientificArticle
dc.publisherThe Geological Society of Finland
dc.publisher.countryFinlanden_GB
dc.publisher.countrySuomifi_FI
dc.publisher.country-codeFI
dc.relation.doi10.17741/bgsf/95.1.001
dc.relation.ispartofjournalBulletin of the Geological Society of Finland
dc.relation.issue1
dc.relation.volume95
dc.source.identifierhttps://www.utupub.fi/handle/10024/183546
dc.titleMultiscale interpretation and scaling analysis of the censored brittle structural framework within the crystalline bedrock of Southern Finland
dc.year.issued2023

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