dc.date.accessioned | 2020-11-27T20:44:06Z | |
dc.date.available | 2020-11-27T20:44:06Z | |
dc.date.created | 2020-11-11T15:41:58Z | |
dc.date.issued | 2020 | |
dc.identifier.citation | Braathen, Alvar petrie, elisabeth Nystuen, Tonje Sundal, Anja Skurtveit, Elin Zuchuat, Valentin Gutierrez, Marte Midtkandal, Ivar . Interaction of deformation bands and fractures during progressive strain in monocline - San Rafael Swell, Central Utah, USA. Journal of Structural Geology. 2020, 141 | |
dc.identifier.uri | http://hdl.handle.net/10852/81193 | |
dc.description.abstract | Folds in porous sandstone in cases allow identification of progressive deformation in an evolving strain field. In the Navajo Sandstone of the km-scale Laramide-style monocline of the San Rafael Swell (Utah, USA), four populations of small-scale structures record different kinematics and deformation mechanisms, depending on orientation to bedding within the first-order fold. Small-scale structures span from cataclastic (shear-) compaction and shear-isochoric deformation bands to dominant disaggregation (shear-) dilation bands. Extension and shear fractures record transformations from band to fracture formation, adding to the structural diversity.
Early structures record semi-penetrative shear deformation guided by bedding and lamination in eolian deposits, consistent with layer-parallel shortening. Subsequent deformation is localized and at a higher angle relative to bedding, recording forward-directed and subsequently backward-directed shear structures within the east-verging monocline. Final deformation is highly localized and appears as a conjugate set of sub-vertical shear zones with shortening-extension axes oblique to the monocline.
For the given conditions in a progressive shear system in highly porous sandstones, interactions of deformation bands and fractures suggest a revival of deformation bands by mutual shear band-fracture systems as developing band swarms rotate into an extensional strain sector during folding. In cases of deformation by shear-dilation strain, deformation bands may evolve directly into fractures, as grain contacts are lost. | |
dc.language | EN | |
dc.rights | Attribution 4.0 International | |
dc.rights.uri | https://creativecommons.org/licenses/by/4.0/ | |
dc.title | Interaction of deformation bands and fractures during progressive strain in monocline - San Rafael Swell, Central Utah, USA | |
dc.type | Journal article | |
dc.creator.author | Braathen, Alvar | |
dc.creator.author | petrie, elisabeth | |
dc.creator.author | Nystuen, Tonje | |
dc.creator.author | Sundal, Anja | |
dc.creator.author | Skurtveit, Elin | |
dc.creator.author | Zuchuat, Valentin | |
dc.creator.author | Gutierrez, Marte | |
dc.creator.author | Midtkandal, Ivar | |
cristin.unitcode | 185,15,22,50 | |
cristin.unitname | Seksjon for geologi og geofysikk | |
cristin.ispublished | true | |
cristin.fulltext | original | |
cristin.qualitycode | 2 | |
dc.identifier.cristin | 1847050 | |
dc.identifier.bibliographiccitation | info:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Journal of Structural Geology&rft.volume=141&rft.spage=&rft.date=2020 | |
dc.identifier.jtitle | Journal of Structural Geology | |
dc.identifier.volume | 141 | |
dc.identifier.pagecount | 16 | |
dc.identifier.doi | https://doi.org/10.1016/j.jsg.2020.104219 | |
dc.identifier.urn | URN:NBN:no-84265 | |
dc.type.document | Tidsskriftartikkel | |
dc.type.peerreviewed | Peer reviewed | |
dc.source.issn | 0191-8141 | |
dc.identifier.fulltext | Fulltext https://www.duo.uio.no/bitstream/handle/10852/81193/4/1-s2.0-S0191814120304399-main.pdf | |
dc.type.version | PublishedVersion | |
cristin.articleid | 104219 | |
dc.relation.project | NFR/244049 | |
dc.relation.project | NFR/295061 | |
dc.relation.project | NFR/257579 | |