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Télécharger le fichier - Service géologique de Wallonie

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Formatie van Bois <strong>de</strong>s MouchesZandstenen en siltstenen, soms micahou<strong>de</strong>n<strong>de</strong>, ink<strong>le</strong>ine banken. Kalkhou<strong>de</strong>n<strong>de</strong> tussenlagen.Grofkorrelige kalksteen en zandige kalksteen aan<strong>de</strong> top (Struniaan). Zandsteen in dikken banken an<strong>de</strong> basis van <strong>de</strong> formatieBois <strong>de</strong>s Mouches FormationGey brownish, sometimes micaceous sandstoneand siltstone, more often in small beds. Calcareousintercalations in the upper part (Strunian).FLSAISLUSFalisol<strong>le</strong> FormationGrüner o<strong>de</strong>r bor<strong>de</strong>auxfarbener Schiefer.Kavernöse, hematititischer Bän<strong>de</strong>r mitBrachiopo<strong>de</strong>n. K<strong>le</strong>ine sandige Bänken im oberenTeil <strong>de</strong>r Formation.Formatie van Falisol<strong>le</strong>Groene of ro<strong>de</strong>wijngek<strong>le</strong>ur<strong>de</strong> schiefers.Hematitische knollige ban<strong>de</strong>n met brachiopo<strong>de</strong>n.K<strong>le</strong>in zandsteendige tussenlagen aan <strong>de</strong> top.Falisol<strong>le</strong> FormationBor<strong>de</strong>aux or green sha<strong>le</strong>s. Cavernous beds withhematite and brachiopods. Small sandy beds at thetop of the formation.Aisemont FormationAus verschie<strong>de</strong>nen Tei<strong>le</strong> zusammen<strong>de</strong>setzteFormation grüner Schiefer, die in zweiKalkhorizonte eingeschlossen ist. Bank ausknolligen Schiefer an <strong>de</strong>r Basis : «Banc à pains»aus Phillipsastrea. Biostroma<strong>le</strong> Kalksteinbank mitStromatoporen und rosttroten Dolomietf<strong>le</strong>cken imobere Teil.Formatie van Aisemont.Groene schiefer tussen twee biostroma<strong>le</strong>kalkstenen. Aan <strong>de</strong> bassis, knollige schiefer metPhillipsastrea. Aan <strong>de</strong> top, dikke bank vangebouwd kalksteen met stromatoporen en bruinetaken van dolomiet.Aisemont FormationDual formation composed by green sha<strong>le</strong>s flankedby two horizons of buil<strong>de</strong>d limestone. At the basis,bed of nodular schist «banc à pains» withPhillipsastrea.Lustin FormationWechselfolge massiger Riffkalke undgutgeschichteter KalksteineBiostroma<strong>le</strong> Fazies an <strong>de</strong>r Basis (Marbre SteAnne» - Ste Anne «Marmor). Dolomitisierte Tei<strong>le</strong>und gutgeschichtete feingebän<strong>de</strong>rte Kalksteine109

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