References of "Belanger, I"
     in
Bookmark and Share    
Full Text
See detailCarte hydrogéologique de Wallonie, Bouillon - Dohan, Muno, 67/1-2. 67/6
Bouezmarni, Mohamed ULiege; Belanger, I.; Ghysel, P. et al

Cartographic material (2017)

Detailed reference viewed: 16 (2 ULiège)
Full Text
See detailCarte hydrogéologique de Wallonie, Vivy - Paliseul, 64/5-6 (notice explicative)
Bouezmarni, Mohamed ULiege; Hanson, Alain ULiege; Belanger, I. et al

Book published by SPW - DGARNE - actualisation partielle : septembre 2015 - Première version : septembre 2014 (2015)

Detailed reference viewed: 16 (1 ULiège)
Full Text
See detailCarte hydrogéologique de Wallonie, Vivy - Paliseul, 64/5-6
Bouezmarni, Mohamed ULiege; Hanson, Alain ULiege; Belanger, I. et al

Cartographic material (2015)

Detailed reference viewed: 18 (6 ULiège)
Full Text
See detailNotice explicative de la carte de Messancy-Saint Léger Musson-Le Fays Houwald
Belanger, I.; Delsate, D.; Ghysel, P. et al

Book (2002)

La feuille Saint-Léger – Messancy, Musson – Le Fays et Houwald située en Lorraine belge entre les frontières luxembourgeoise et française couvre l'extrême sud-est de la Belgique. En marge du Bassin de ... [more ▼]

La feuille Saint-Léger – Messancy, Musson – Le Fays et Houwald située en Lorraine belge entre les frontières luxembourgeoise et française couvre l'extrême sud-est de la Belgique. En marge du Bassin de Paris, la région est couverte de roches sédimentaires mésozoïques d'allure monoclinale. Les couches de très faible pendage sud-est sont affectées de nombreuses failles de direction NE-SW à ENE-WSW. L'allure des couches ainsi que la nature contrastée des roches composant le sous-sol lorrain a déterminé un paysage typique de cuestas. Cette structure du relief affectée, dès le Tertiaire, par le climat et le réseau hydrographique cède la place à des vallées asymétriques (région de Saint-Léger), des buttes témoins et des plateaux ou terrasses alluviales. Les témoins de ces événements sont visibles entre autres par les anciennes alluvions et par des cuirassements ferrugineux ou siliceux. Parmi les nombreuses exploitations du sous-sol lorrain, celle du fer a principalement influencé le développement de la région d'Athus. Actuellement seuls le sable et l'eau des différents aquifères sont encore exploités. [less ▲]

Detailed reference viewed: 132 (11 ULiège)
Full Text
Peer Reviewed
See detailNew lithostratigraphical, sedimentological, mineralogical and palaeontological data on the Mesozoic of Belgian Lorraine: a progress report
Boulvain, Frédéric ULiege; Belanger, I.; Delsate, D. et al

in Geologica Belgica (2001), 3(1-2), 3-33

A multidisciplinary study of some extensively cored boreholes together with the new 1/25.000 geological mapping of wallonia lead us to propose a new lithostratigraphic canvas for belgian lorraine. This ... [more ▼]

A multidisciplinary study of some extensively cored boreholes together with the new 1/25.000 geological mapping of wallonia lead us to propose a new lithostratigraphic canvas for belgian lorraine. This area is located on the n-e border of the paris basin, south of the ardennes; the studied stratigraphic interval covers the keuper to the toarcian. Each of the newly defined units is sedimentologicaly interpreted on the basis of macroscopic and microscopic observations. Detailed palynological and claystratigraphical analyses have been performed, providingadditional stratigraphical, palaeoecological and sedimentological data. Moreover, a first sequence stratigraphic interpretation is proposed for this highly transgressive sedimentary body. The habay formation (conglomerates and red mudstones) is a fluvial unit, with immature channel conglomerates and paleosoils; the attert formation (dolomitic marls with gypsum and pseudomorphs) exhibites an evaporitic trend. The Mortinsart formation (sands and marls) corresponds to a restricted marine unit, evolving towards an alluvial plain (levallois member). The second cycle begins with the Jamoigne Formation (bioturbated marls and limestones), a marine subtidal restricted unit, evolving towards a more sandy sedimentary body (Metzert Member). The base of the third cycle corresponds to the rest of the Luxemburg Formation, comprising a succession of sandy waves. The Ethe Formation (laminar mudstones and marls) marks a deepening of the basin and the outset of open marine dysaerobic conditions. The Aubange Formation (bioturbated marls with sandstones and limestones) is characterized by the reappearance of a normal benthic fauna. The Grandcourt Formation (laminar mudstones and marls) marks a return to open marine dysaerobic conditions. The Mont-Saint-Martin Formation (marls, sandy marls and oolitic ironstone) is a highly regressive unit, while the Longwy Formation (limestones) marks the initiation of a carbonate platform. [less ▲]

Detailed reference viewed: 67 (1 ULiège)
Full Text
Peer Reviewed
See detailTriassic and Jurassic lithostratigraphic units (Belgian Lorraine)
Boulvain, Frédéric ULiege; Belanger, I.; Delsate, D. et al

in Geologica Belgica (2001), 4(1-2), 113-119

A multidisciplinary study of some extensively cored boreholes together with the new 1/25,000 geological mapping of Wallonia led us to propose a new lithostratigraphic canvas for Belgian Lorraine. This ... [more ▼]

A multidisciplinary study of some extensively cored boreholes together with the new 1/25,000 geological mapping of Wallonia led us to propose a new lithostratigraphic canvas for Belgian Lorraine. This area is located on the NE border of the Paris Basin, south of the Ardennes; the studied stratigraphic interval covers the Keuper to the Bajocian. [less ▲]

Detailed reference viewed: 68 (3 ULiège)