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Active tectonics, seismicity and geomorphology with special reference to Normandy (France)

✍ Scribed by Jean-Louis Lagarde; Stéphane Baize; Daniel Amorese; Bernard Delcaillau; Marianne Font; Philippe Volant


Book ID
101351596
Publisher
John Wiley and Sons
Year
2000
Tongue
English
Weight
475 KB
Volume
15
Category
Article
ISSN
0267-8179

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✦ Synopsis


Integrated studies based on tectonic, seismotectonic and geomorphological analyses indicate that Normandy (northwest France) has been an active area during the Quaternary. Topography and landform discontinuities reflect the dislocation and differential uplift of a late Cenozoic platform. The tectonic activity is represented by (i) active faults, indicated by linear scarps and seismic activity, (ii) offsetting of pre-existing surfaces, (iii) Plio-Pleistocene sedimentation restricted within narrow subsiding zones, and (iv) morphometric properties of drainage basins that indicate zones of differential uplift. The inferred strain pattern involves (i) a shortening direction that strikes NW-SE as expected in the European context of Alpine compression, and (ii) a NE-SW trending extension accommodated by NW-SE normal faults. The geomorphological systems encountered in Normandy preferentially record differential vertical displacements.


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