The occurrence of Dickinsonia in non-marine facies
Dickinsonia in the central Urals occurs in a succession transitional from marginal marine to non-marine. Even within this sequence Dickinsonia appears to be restricted to the least marine facies interpreted as a coastal lagoon surrounded by tidal flats. Another puzzling aspect is the complete absenc...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Consejo Superior de Investigaciones Científicas
2019-12-01
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| Series: | Estudios Geologicos |
| Subjects: | |
| Online Access: | http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/989 |