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 |
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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 |
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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 |
eng |
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 |
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dc.description.version |
publishedVersion |
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tib.accessRights |
frei zug�nglich |
|