Triassic conodonts of the Slovenian Basin

Slovenian Basin was formed during the Ladinian following disintegration of the Slovenian Carbonate Platform. It persisted continuously until the Late Cretaceous. Several conodont asscociations were recognized within the Triassic rocks of the Slovenian Basin. Stratigraphically significant species bel...

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Bibliographic Details
Main Authors: Stanko Buser, Tea Kolar-Jurkovšek, Bogdan Jurkovšek
Format: Article
Language:English
Published: Geological Survey of Slovenia 2007-06-01
Series:Geologija
Subjects:
Online Access:http://www.geologija-revija.si/dokument.aspx?id=337