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- W234769319 abstract "Reconstruction of the original, immediately-afterimpact, crater is performed for Mjolnir, Chicxulub and Bosumtwi craters by decompaction and fault restoration, as the three craters represent upper and lower range cases in the aspect of the experienced level of post-impact overburden. The Mjolnir crater currently lies beneath ~50-800 m of post-impact sediments (Fig. 1f) [e.g. 1]. Of major importance in the reconstruction analysis is the fact that about 1.5-2 km of siliciclastic sediments were deposited during Cretaceous-Tertiary times (Fig. 1d) [e.g. 2] and were later removed, including the top of the central high (Fig. 1e), during the Late Cenozoic glacial erosion. Reconstruction suggests that the impact resulted in a very shallow structure with an average crater depth of only ~30 m (Fig. 1a)." @default.
- W234769319 created "2016-06-24" @default.
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- W234769319 date "2007-03-01" @default.
- W234769319 modified "2023-09-26" @default.
- W234769319 title "Reconstruction of the Original Impact-Crater Relief for Mjølnir, Chicxulub and Bosumtwi Impact Craters Reveals Surprisingly Shallow Structures: Did We Miss Something?" @default.
- W234769319 hasPublicationYear "2007" @default.
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