2020
DOI: 10.5880/gfz.dekorp-1a.001
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Deep seismic reflection profile DEKORP 1987-1A across the western Rhenish Massif, West Germany/ East Belgium

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“…All these faults could be connected at several kilometers in-depth to the Midi-Eifel thrust fault, a major thrust fault corresponding to the northernmost front of the Variscian Orogeny and connecting both regions. This fault acts as an important seismic reflector and could thus be observed below the Stavelot Massif thanks to seismic measurements surveys lead by the DEKORP research group in the early nineties (Stiller et al 1987).…”
Section: Discussionmentioning
confidence: 99%
“…All these faults could be connected at several kilometers in-depth to the Midi-Eifel thrust fault, a major thrust fault corresponding to the northernmost front of the Variscian Orogeny and connecting both regions. This fault acts as an important seismic reflector and could thus be observed below the Stavelot Massif thanks to seismic measurements surveys lead by the DEKORP research group in the early nineties (Stiller et al 1987).…”
Section: Discussionmentioning
confidence: 99%