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- W1978803709 abstract "Tsunamis are unexpected, violent events and can rarely be studied by direct observation, so that much of their hydrodynamic behaviour is uncertain. Careful examination of their deposits can therefore assist in determining flow conditions and depositional processes (Le Roux and Vargas, 2005), but a prerequisite is that such deposits be identified correctly. In our opinion, the paper by Fujino et al. (2006) does not meet this criterion. The authors mention five features that, according to them, can only co-exist if they were formed by a tsunami, although they admit that each of these features individually may be attributed to other processes. Here we contend that all five features can occur together in a wave-dominated, shallow marine environment affected by storms. Imbrication reflecting current reversals from seawardto landward-directed is attributed byFujino et al. (2006) to the onrush and backwash of successive waves during a single event. Because the environment was wavedominated, as shown by an abundance of hummocky cross-stratified (HCS) sandstones, they rule out tidal action as a possible cause. However, strong wave action" @default.
- W1978803709 created "2016-06-24" @default.
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- W1978803709 date "2007-10-01" @default.
- W1978803709 modified "2023-10-14" @default.
- W1978803709 title "Structure and depositional processes of a gravelly tsunami deposit in a shallow marine setting: Lower Cretaceous Miyako Group, Japan—discussion" @default.
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- W1978803709 doi "https://doi.org/10.1016/j.sedgeo.2007.04.002" @default.
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