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- W2014374791 abstract "An interesting phenomenon above some classic geological structures can be observed on many seismic sections. Namely, a part of the seismic horizon appears downthrown by normal faults to a position deeper than the flanks. The downthrown part of the horizon is above the shallowest parts of the classic antiform." @default.
- W2014374791 created "2016-06-24" @default.
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- W2014374791 date "1994-01-01" @default.
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- W2014374791 title "Collapsed geologic structures" @default.
- W2014374791 doi "https://doi.org/10.3997/2214-4609.201410227" @default.
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