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- W2068207513 abstract "Abstract A number of NW-SE or NNW-SSE trending radial faults are recognized on the northern slope of the Ardenne massif. They have been active since the Oligocene, as depicted by deformations of planation surfaces and other morphological features. The study of river terraces demonstrates their Quaternary activity, with vertical movements ranging from 4 to 10 m during the late Quaternary. This fault activity is related to the opening of the Lower Rhine Embayment." @default.
- W2068207513 created "2016-06-24" @default.
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- W2068207513 date "1989-07-01" @default.
- W2068207513 modified "2023-09-27" @default.
- W2068207513 title "Quaternary tectonics in the northern Ardennes, Belgium" @default.
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- W2068207513 doi "https://doi.org/10.1016/0040-1951(89)90266-7" @default.
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