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Publikováno v:
Geologica Belgica. 24:159-167
The sandy Zandvliet Member represents a particular, decalcified facies in the top of the Pliocene Lillo Formation in northern Belgium. Based on the correlation with nearby boreholes at the type locality of the Zandvliet Member, we were able to charac
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6db4c49c279f8776097be9d894fb2379
https://doi.org/10.20341/gb.2021.006
https://doi.org/10.20341/gb.2021.006
