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pro vyhledávání: '"Belgium, Anhée"'
The Moliniacian is the basal division of the Viséan in Belgium (regional Substage). Its base is identified by the entry of the foraminifer Eoparastaffella simplex in the Salet road section and correlates with the base of the Viséan Stage. Its top i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______232::df768940ce185e17da75526101eedde5
http://www.vliz.be/imisdocs/publications/241995.pdf
http://www.vliz.be/imisdocs/publications/241995.pdf
The Warnantian Substage is about 8 to 12 Ma long and was defined as corresponding to the Cf6 Foraminifer Zone by Conil et al., 1977 (= MFZ13 to MFZ15 Zones of Devuyst & Hance (in Poty et al., in press). Its base is taken at the base of the Bonne Rive
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______232::d5f02ef0af9bcf3121f947e39d09b666
http://www.vliz.be/imisdocs/publications/242001.pdf
http://www.vliz.be/imisdocs/publications/242001.pdf
Autor:
Mottequin, B
Paleoecology and sedimentological interpretation of the "black marble" of Denée (Lower Visean; Belgium). The paleoecology of the "black marble" of Denée (Dinant sedimentation area (DSA), Belgium) is reviewed in light of recent paleoecological, taph
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______232::bec503ea6c2fbeee6bd99687fa4399aa
http://www.vliz.be/imisdocs/publications/242018.pdf
http://www.vliz.be/imisdocs/publications/242018.pdf
Autor:
Bultynck, P., Coen-Aubert, M., Dejonghe, L., Godefroid, J., Hance, L., Lacroix, D., Préat, A., Stainier, P., Steemans, P., Streel, M., Tourneur, F.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______232::3c9b312e3712ee041fdd109bf1710497
http://www.vliz.be/imisdocs/publications/251664.pdf
http://www.vliz.be/imisdocs/publications/251664.pdf
Autor:
Mamet, B.
This study works out the sedimentation of upper paleozoic formations of Belgium and northern France.It deals with sequential analysis of calcareous facies, more particularily, the so-called « black marbles »; it is possible to recognize a number of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______232::ec96450eb487834cf19f2617cdefb50f
http://www.vliz.be/imisdocs/publications/252011.pdf
http://www.vliz.be/imisdocs/publications/252011.pdf