Frasnian (Upper Devonian) lithostratigraphy of the Bernesga Valley (Cantabrian Mountains, NW Spain)
Sequence stratigraphic units are defined in terms of changes in relative sea level, and not on the compositional similarity of the lithology of the rock units. Sequence boundaries were used to support the formal definitions of the Gordón Member and the Millar Member of the Frasnian Nocedo Formation...
| Published in: | Geologos |
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| Main Author: | |
| Format: | Article |
| Language: | English |
| Published: |
Sciendo
2025-08-01
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| Subjects: | |
| Online Access: | https://doi.org/10.14746/logos.2025.31.2.09 |