Spor etter Mjølnirnedslaget i Janusfjellprofilet på Svalbard

The 40 km diameter Mjølnir Crater was formed 142 ± 2.6 Ma (Volgian-Ryazanian boundary) by the impact of a 1.6 km diameter asteroid into the 350-400 m deep paleo-Barents Sea. The structure is buried and well preserved in sediments on the Bjarmeland Platform, which has been tectonically stable since l...

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Bibliographic Details
Main Author: Salvigsen, Ottar
Other Authors: Førsteamanuensis Henning Dypvik
Format: Master Thesis
Language:Norwegian Bokmål
Published: 2004
Subjects:
VDP::450
Agardhfjellet
Barents Sea
Janusfjellet
Myklegardfjellet
Rurikfjellet
Slottsmøya
Svalbard
Wimanfjellet
Siberia
Online Access:http://hdl.handle.net/10852/12347
http://urn.nb.no/URN:NBN:no-9224

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