The Mesozoic-Cenozoic tectonic evolution of the New Siberian Islands, NE Russia

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dc.identifier.uri http://dx.doi.org/10.15488/2360
dc.identifier.uri http://www.repo.uni-hannover.de/handle/123456789/2386
dc.contributor.author Brandes, Christian
dc.contributor.author Piepjohn, Karsten
dc.contributor.author Franke, Dieter
dc.contributor.author Sobolev, Nikolay
dc.contributor.author Gaedicke, Christoph
dc.date.accessioned 2017-11-17T12:10:55Z
dc.date.available 2017-11-17T12:10:55Z
dc.date.issued 2015
dc.identifier.citation Brandes, C.; Piepjohn, K.; Franke, D.; Sobolev, N.; Gaedicke, C.: The Mesozoic-Cenozoic tectonic evolution of the New Siberian Islands, NE Russia. In: Geological Magazine 152 (2015), Nr. 3, S. 480-491. DOI: https://doi.org/10.1017/S0016756814000326
dc.description.abstract On the New Siberian Islands the rocks of the east Russian Arctic shelf are exposed and allow an assessment of the structural evolution of the region. Tectonic fabrics provide evidence of three palaeo-shortening directions (NE–SW, WNW–ESE and NNW–SSE to NNE–SSW) and one set of palaeo-extension directions revealed a NE–SW to NNE–SSW direction. The contractional deformation is most likely the expression of the Cretaceous formation of the South Anyui fold–thrust belt. The NE–SW shortening is the most prominent tectonic phase in the study area. The WNW–ESE and NNW–SSE to NNE–SSW-oriented palaeo-shortening directions are also most likely related to fold belt formation; the latter might also have resulted from a bend in the suture zone. The younger Cenozoic NE–SW to NNE–SSW extensional direction is interpreted as a consequence of rifting in the Laptev Sea. eng
dc.language.iso eng
dc.publisher Cambridge : Cambridge University Press
dc.relation.ispartofseries Geological Magazine 152 (2015), Nr. 3
dc.rights Es gilt deutsches Urheberrecht. Das Dokument darf zum eigenen Gebrauch kostenfrei genutzt, aber nicht im Internet bereitgestellt oder an Außenstehende weitergegeben werden. Dieser Beitrag ist aufgrund einer (DFG-geförderten) Allianz- bzw. Nationallizenz frei zugänglich.
dc.subject De Long Islands eng
dc.subject fold-thrust belt eng
dc.subject New Siberian Islands eng
dc.subject South Anyui suture zone eng
dc.subject Cenozoic eng
dc.subject deformation eng
dc.subject extensional tectonics eng
dc.subject fold and thrust belt eng
dc.subject Mesozoic eng
dc.subject rifting eng
dc.subject suture zone eng
dc.subject tectonic evolution eng
dc.subject tectonic setting eng
dc.subject De Long Islands eng
dc.subject New Siberian Islands eng
dc.subject Russian Federation eng
dc.subject Sakha eng
dc.subject.ddc 550 | Geowissenschaften ger
dc.title The Mesozoic-Cenozoic tectonic evolution of the New Siberian Islands, NE Russia
dc.type article
dc.type Text
dc.relation.issn 0016-7568
dc.relation.doi https://doi.org/10.1017/S0016756814000326
dc.bibliographicCitation.issue 3
dc.bibliographicCitation.volume 152
dc.bibliographicCitation.firstPage 480
dc.bibliographicCitation.lastPage 491
dc.description.version publishedVersion
tib.accessRights frei zug�nglich


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