2018
DOI: 10.1134/s0016852118060067
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Structure of the Laptev Sea Shelf–Eurasian Basin Transition Zone (Arctic Ocean)

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Cited by 8 publications
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“…This applies, in particular, to the Eurasian Basin where the Cenozoic linear magnetic anomalies are common in the Amundsen and Nansen basins, while the age of the lower horizons of the sedimentary cover over most of the area is estimated as Lower-Upper Cretaceous, or even Jurassic (near East Taimyr) [24]. Within the perioceanic troughs, even older complexes are sometimes traced [25,26], to the Paleozoic ones [27].…”
mentioning
confidence: 99%
“…This applies, in particular, to the Eurasian Basin where the Cenozoic linear magnetic anomalies are common in the Amundsen and Nansen basins, while the age of the lower horizons of the sedimentary cover over most of the area is estimated as Lower-Upper Cretaceous, or even Jurassic (near East Taimyr) [24]. Within the perioceanic troughs, even older complexes are sometimes traced [25,26], to the Paleozoic ones [27].…”
mentioning
confidence: 99%