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dc.contributor.authorKlokočník, Jaroslav
dc.contributor.authorKostelecký, Jan
dc.contributor.authorBezděk, Aleš
dc.contributor.authorKletetschka, Gunther
dc.contributor.authorStaňková, Hana
dc.date.accessioned2020-05-22T06:13:34Z
dc.date.available2020-05-22T06:13:34Z
dc.date.issued2020
dc.identifier.citationScientific Reports. 2020, vol. 10, issue 1, art. no. 6093.cs
dc.identifier.issn2045-2322
dc.identifier.urihttp://hdl.handle.net/10084/139498
dc.description.abstractWe provide arguments in favour of impact origin of a 200 km suspected impact crater Kotuykanskaya near Popigai, Siberia, Russia. We use the gravity aspects (gravity disturbances, the Marussi tensor of the second derivatives of the disturbing geopotential, the gravity invariants and their specific ratio, the strike angles and the virtual deformations), all derived from the combined static gravity field model EIGEN 6C4, with the ground resolution of about 10 km and a precision of about 10 milliGals. We also use the magnetic anomalies from the model EMAG2 and emphasize the evidence of much deeper sources in the suspected area, constraining the impact origin of this structure.cs
dc.language.isoencs
dc.publisherSpringer Naturecs
dc.relation.ispartofseriesScientific Reportscs
dc.relation.urihttp://doi.org/10.1038/s41598-020-62998-6cs
dc.rightsCopyright © 2020, Springer Naturecs
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/cs
dc.titleA 200 km suspected impact crater Kotuykanskaya near Popigai, Siberia, in the light of new gravity aspects from EIGEN 6C4, and other datacs
dc.typearticlecs
dc.identifier.doi10.1038/s41598-020-62998-6
dc.rights.accessopenAccesscs
dc.type.versionpublishedVersioncs
dc.type.statusPeer-reviewedcs
dc.description.sourceWeb of Sciencecs
dc.description.volume10cs
dc.description.issue1cs
dc.description.firstpageart. no. 6093cs
dc.identifier.wos000529507400001


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