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Peer Reviewed
See detailKarel ende Elegast et la tradition folklorique
Varvaro, Alberto; Moreno, Paola ULg

in Moyen Age (Le) (1995), CI(1995), 259-275

Detailed reference viewed: 66 (3 ULg)
See detail«Karel ende Elegast et la tradition folklorique»
Moreno, Paola ULg

Book (1995)

Detailed reference viewed: 10 (7 ULg)
See detailKarel Tchapek : humaniste et visionnaire
Mouton, Charles ULg

in Revue Générale (1995), (6/7), 71-80

Detailed reference viewed: 18 (0 ULg)
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See detailKarenoïdne izdeliya paleoliticheskoï stoyanki Kulbulak: opit tekhniko-tipologicheskoï klassifikatsii
Kolobova, K.; Krivoshapkin, A.; Flas, Damien ULg et al

in Vestnik NGU. Seriâ Istoriâ, Filologiâ (2011), 10(7), 87-99

Detailed reference viewed: 8 (1 ULg)
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Peer Reviewed
See detailKarenwebberite, Na(Fe,Mn)2+PO4, a new phosphate mineral species from the Malpensata pegmatite, Lecco province, Italy.
Vignola, P; Hatert, Frédéric ULg; Fransolet, André-Mathieu ULg et al

in PEG2013 – 6th International Symposium on Granitic Pegmatites, Abstract book (2013)

Detailed reference viewed: 21 (0 ULg)
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Peer Reviewed
See detailKarenwebberite, Un nuovo fosfato primario dal filone megmatitico della Malpensata, Colico, Lecco
Vignola, P; Hatert, Frédéric ULg; Fransolet, André-Mathieu ULg et al

in Rivista mineralogica italiana (2013), 4/2013

Detailed reference viewed: 25 (3 ULg)
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See detailKarl Marx, Œuvres, IV, Politique I
Durand, Pascal ULg

in Avancées (1995)

Detailed reference viewed: 22 (5 ULg)
See detailDe Karmelietenkerk in Gent, Dendrochronologische analyse van de dakconstructie boven tweede beuk
Hoffsummer, Patrick ULg; Houbrechts, David

in Stadsarcheologie (1995), 18(2),

Detailed reference viewed: 37 (1 ULg)
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Peer Reviewed
See detailKarst dans les évaporites : marqueur efficace des événements récents. L’exemple du Mont Sédom (Israel)
Hallot, Eric ULg

in Bulletin de la Société Géographique de Liège (1999), 37

Detailed reference viewed: 26 (4 ULg)
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See detailKarst dans les micaschistes d'Akok Bekoé - Sud Cameroun
Willems, Luc ULg; Vicat, Jean-Paul; Pouclet, André

in Bulletin de la Société Géographique de Liège (1999), 37(2), 5-18

50 km south of Yaoundé, karst phenomena are developed in micaschists. A network of fractures dependent in thrusting area guided formation of caves, conduits and other morphologies comparable with those ... [more ▼]

50 km south of Yaoundé, karst phenomena are developed in micaschists. A network of fractures dependent in thrusting area guided formation of caves, conduits and other morphologies comparable with those found in the karst limestones. The presence of a spring and the proximity of the Nyong river suggest that a chemical erosion within an aquifer is at the origin of most of forms. The position of certain conduits and tafonis dismisses the assumption of a genesis within a weathering mantle. [less ▲]

Detailed reference viewed: 28 (1 ULg)
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See detailKarst et CO2. Le transfert de CO2 dans le synclinal carbonifère de Comblain-au-Pont
Ek, Camille ULg; Godissart, Jean

in Ecokarst (2013), 92

CO2, solved in water, is the main factor of karstification. In the caves, CO2 concentration in air raises commonly up to 10 000 ppm and, during summertime, 20 000 and more.

Detailed reference viewed: 22 (4 ULg)
See detailKarst et hydrologie
Petit, François ULg

Book (1999)

Detailed reference viewed: 13 (2 ULg)
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Peer Reviewed
See detailKarst in granitic rocks, South Cameroon: cave genesis and silica and taranakite speleothems
Willems, Luc ULg; Compère, Philippe ULg; Hatert, Frédéric ULg et al

in Terra Nova (2002), 14(5), 355-362

A cave in granitic rocks was studied in Mezesse, South Cameroon. Coralloid speleothems, draperies and dissolution traces on the cave walls attest to its truly karstic nature. The speleothems consist of ... [more ▼]

A cave in granitic rocks was studied in Mezesse, South Cameroon. Coralloid speleothems, draperies and dissolution traces on the cave walls attest to its truly karstic nature. The speleothems consist of microlayers of opal and taranakite (K,NH4)Al-3(PO4)(3)(OH).9H(2)O. They indicate a significant mobilization of silica, Al and K from granite during the formation of the cave. Identification of silicified bacteria in the speleothems layers suggests a possible role of these micro-organisms in silica deposition. The presence of taranakite and of silicified organic remains within the speleothems lead to a better understanding of the genesis of the cave. [less ▲]

Detailed reference viewed: 142 (24 ULg)
See detailKarst in het krijt van Limburg en ombeving
Lagrou, David; Dusart; Willems, Luc ULg

Poster (2008)

Detailed reference viewed: 22 (0 ULg)
Peer Reviewed
See detailKarst non carbonaté au Cameroun méridional. L'exemple des grottes de Mfoula
Willems, Luc ULg; Pouclet, André; Vicat, Jean-Paul

in Würzburger Geographische Arbeiten (1997), 89

Detailed reference viewed: 13 (0 ULg)
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See detailLe karst
Ek, Camille ULg; Schyns, Jean-Christophe; Ozer, André ULg

in Direction générale de l'aménagement du territoire, du logement et du patrimoine (Ed.) Les risques majeurs en Région wallonne (2006)

Detailed reference viewed: 156 (41 ULg)
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Peer Reviewed
See detailKarstification souterraine en milieu saturé
Briffoz, Albert; Ek, Camille ULg; Gewelt, Michel

in Annales de la Société Géologique de Belgique (1985), 108

In order to explain the development of caves, considering the slowness of water circulations into the fissures of the limestone, only a chemical action i.e. corrosion can be called upon in most cases ... [more ▼]

In order to explain the development of caves, considering the slowness of water circulations into the fissures of the limestone, only a chemical action i.e. corrosion can be called upon in most cases. However, as saturation is rapidly reached, we consider, in order to extend the dissolution action of underground water, the possibility of dissolution in a saturated environment. [less ▲]

Detailed reference viewed: 29 (7 ULg)
See detailKarsts dans les gneiss - alvéoles géantes et micro-alvéoles dans la région de Milagres, état de Bahia, Brésil
Rodet, Joël; Willems, Luc ULg; Auler, Augusto

Conference (2009, December 05)

Detailed reference viewed: 15 (1 ULg)