The Tohogne borehole section, from the Lower Tournaisian into the Upper Famennian, has a remarkable micropalaeontological content (conodonts, foraminifers, spores) which enabled a detailed subdivision of these strata. New data in biostratigraphy and systematic palaeontology and palaeogeographic implications are presented, as well as correlations with reference sections.
All data in the Integrated Marine Information System (IMIS) is subject to the VLIZ privacy policy
Web site hosted and maintained by Flanders Marine Institute (VLIZ)
Webmaster info@vliz.be Number of visitors: 1092918 - Total hits: 7338436 (since 2006-01-17)