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Het Tertiair tussen Gent en Overmere
Jacobs, P. (1973). Het Tertiair tussen Gent en Overmere. Natuurwet. Tijdschr. 55(8): 229-243
In: Natuurwetenschappelijk Tijdschrift. L. Walschot/Natuur- en Geneeskundige Vennootschap: Gent. ISSN 0770-1748, more
Peer reviewed article  

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    Deposition features
    Geological time > Phanerozoic > Geological time > Cenozoic > Tertiary
    ANE, Belgium [Marine Regions]

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    The Tertiary substratum between Ghent and Overmere (East Flanders, Belgium) consists of subhorizontal layers of Ypresian, Paniselian, Ledian and Bartonian age, which represent almost the entire Eocene, except the Bruxellian. A description of the facies and the sedimentological features of the sediments is given. A hypsometric map of the top of the Tertiary formations and a geological map of the studied area have been compiled from all available informations.

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