Faults in the Asquempont area, southern Brabant Massif, Belgium
Abstract The literature suggests that the Asquempont fault, a supposedly important reverse fault forming the limit between the Lower to lower Middle Cambrian and the Ordovician in the Sennette valley, is poorly understood. Nevertheless, this fault is commonly equated with a pronounced NW-SE-trending aeromagnetic lineament, the Asquempont lineament, and both the geometry of the Asquempont lineament and the supposed reverse movement of the Asquempont fault are used to develop large-scale tectonic models of the Brabant Massif. New outcrop observations in the Asquempont area, the “type locality” o... Mehr ...
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Dokumenttyp: | Artikel |
Erscheinungsdatum: | 2004 |
Reihe/Periodikum: | Netherlands Journal of Geosciences - Geologie en Mijnbouw ; volume 83, issue 1, page 49-66 ; ISSN 0016-7746 1573-9708 |
Verlag/Hrsg.: |
Cambridge University Press (CUP)
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Sprache: | Englisch |
Permalink: | https://search.fid-benelux.de/Record/base-27380654 |
Datenquelle: | BASE; Originalkatalog |
Powered By: | BASE |
Link(s) : | http://dx.doi.org/10.1017/s0016774600020461 |