Middle and Upper Ordovician Strata at Lindegård in the Fågelsång District, Scania, S. Sweden
- 1 February 1961
- journal article
- research article
- Published by Taylor & Francis in Geologiska Föreningen i Stockholm Förhandlingar
- Vol. 83 (1) , 79-85
- https://doi.org/10.1080/11035896109449584
Abstract
A brief description is given of a boring through the Tretaspis series and the uppermost portion of the Chasmops series in the Fågelsång district. The examined portions of the Chasmops series agree with the corresponding strata in Bornholm. The Tretaspis strata which hitherto had been almost unknown in the area consist mainly of pale mudstones and shales including black graptolitiferous layers. They exhibit remarkable similarities with the Moffat series in Scotland and the sequence from Brzezinki in Poland. The following subdivisions are distinguished (from below upwards): 1) Zone of Tretaspis granulata; 2) Zone of Dicellograptus anceps; 3) Practically unfossiliferous mudstones for which the term Lindegård mudstone is proposed.Keywords
This publication has 2 references indexed in Scilit:
- Correlation of the Scandinavian Middle Ordovician with the graptolite successionGeologiska Föreningen i Stockholm Förhandlingar, 1954
- The Moffat SeriesQuarterly Journal of the Geological Society, 1878