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Conodont biostratigraphy of the Oandu Stage (Katian, Upper Ordovician) in NE Estonia

Conodonts from the type region of the Oandu Regional Stage (Katian, Upper Ordovician) in NE Estonia were studied. Here, the lower boundary of the stage corresponds to a discontinuity surface at the base of the Hirmuse Formation and, in conodont succession, is marked by the disappearance of Semiacont...

Disgrifiad llawn

Wedi'i Gadw mewn:
Manylion Llyfryddiaeth
Prif Awdur: Peep Männik
Fformat: Artigo
Iaith:Inglês
Cyhoeddwyd: Estonian Academy Publishers 2017-02-01
Cyfres:Estonian Journal of Earth Sciences
Pynciau:
Mynediad Ar-lein:http://www.kirj.ee/public/Estonian_Journal_of_Earth_Sciences/2017/issue_1/earth-2017-1-1-12.pdf
Tagiau: Ychwanegu Tag
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