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dc.date.accessioned2020-08-13T18:12:01Z
dc.date.available2020-08-13T18:12:01Z
dc.date.created2020-04-30T13:36:30Z
dc.date.issued2020
dc.identifier.citationSolovyeva, M Akhmanov, G Mazzini, Adriano Khabuev, A Khlystov, Oleg . The Gydratny Fault zone of Lake Baikal. Limnology and freshwater biology. 2020, 1, 368-373
dc.identifier.urihttp://hdl.handle.net/10852/78347
dc.description.abstractThe Central basin of Lake Baikal is intersected by the North-East – South-West-oriented escarpment named the «Gydratny Fault zone». This laterally extensive structure runs subparallel to the North-Western shore of the lake. The Gydratny Fault zone has been investigated using geophysical techniques during 6 years of research in the framework of international expeditions of the Class@Baikal project. The acquired seismic data provided details of the structure of the upper part of the sedimentary section revealing a system of previously unknown faults. A new tectonic scheme of the South-Western deep-water part of the Central basin is presented. The Gydratny fault is accompanied by a system of numerous synthetic and antithetic normal faults that form a wide and extended faulted zone. These structures are unevenly distributed, and include modern and active faults as well as features buried under undeformed sedimentary units with different thickness. This parameter is used to constrain the patterns observed in several zones of the study area. The difference in the characteristics of faults and their manifestations on seismic data can be explained by complex and uneven distribution of active tectonic and sedimentary processes.
dc.languageEN
dc.rightsAttribution-NonCommercial 4.0 International
dc.rights.urihttps://creativecommons.org/licenses/by-nc/4.0/
dc.titleThe Gydratny Fault zone of Lake Baikal
dc.typeJournal article
dc.creator.authorSolovyeva, M
dc.creator.authorAkhmanov, G
dc.creator.authorMazzini, Adriano
dc.creator.authorKhabuev, A
dc.creator.authorKhlystov, Oleg
cristin.unitcode185,15,22,40
cristin.unitnameSenter for Jordens utvikling og dynamikk
cristin.ispublishedtrue
cristin.fulltextoriginal
dc.identifier.cristin1808876
dc.identifier.bibliographiccitationinfo:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Limnology and freshwater biology&rft.volume=1&rft.spage=368&rft.date=2020
dc.identifier.jtitleLimnology and freshwater biology
dc.identifier.volume1
dc.identifier.issue1
dc.identifier.startpage368
dc.identifier.endpage373
dc.identifier.doihttps://doi.org/10.31951/2658-3518-2020-A-1-368
dc.identifier.doihttps://doi.org/10.31951/2658-3518-2020-A-1-368
dc.identifier.urnURN:NBN:no-81460
dc.type.documentTidsskriftartikkel
dc.type.peerreviewedPeer reviewed
dc.source.issn2658-3518
dc.identifier.fulltextFulltext https://www.duo.uio.no/bitstream/handle/10852/78347/2/Solovyeva_2020_LFB_Baikal_Gydratny.pdf
dc.type.versionPublishedVersion
dc.relation.projectNFR/288299


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