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- W89128336 abstract "Although protective at initial stages, extensive burial and associated processes, such as mechanical- and chemical-compaction, and diagenesis, may eventually lead to considerable changes in the original crater structure and morphology. Extensive postimpact modifications may obscure many marine impact craters formed in sedimentary, water-covered targets. The same postimpact processes may result in alterations in typical/expected geophysical signatures at such structures. The postimpact structural and morphological crater modification is, generally, an overlooked process because planetary research of impact structures (where postimpact sediment loading is mostly absent) dominated the impact-related research until recently. In addition, the terrestrial impact record is dominated by crystalline-target impacts on land (e.g., Melosh 1989; Ormo and Lindstrom 2000; Dypvik et al. 2004a; Turtle et al. 2005). Furthermore, postimpact modifications are difficult to quantify if an extensive and dense geophysical dataset of seismic reflection profiles and potential field data is not available, which is most commonly the case." @default.
- W89128336 created "2016-06-24" @default.
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- W89128336 date "2010-01-01" @default.
- W89128336 modified "2023-09-26" @default.
- W89128336 title "Postimpact Deformation Due to Sediment Loading: The Mjølnir Paradigm" @default.
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- W89128336 doi "https://doi.org/10.1007/978-3-540-88260-2_9" @default.
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