Bashkirian meganticlinorium: Late Riphean-Vendian hiatuses and possible transformations of basin provenances
The object of research. At the top of the Upper Riphean-Vendian sedimentary sequence of the Bashkirian meganticlinorium (western and central parts of the named structure, corresponding to the stratotypical locality of Riphean) there is a series of fairly well-established hiatuses – the pre-Uk and pr...
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| Autor principal: | |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
A.N. Zavaritsky Institute of Geology and Geochemistry
2020-08-01
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| coleção: | Литосфера |
| Assuntos: | |
| Acesso em linha: | https://www.lithosphere.ru/jour/article/view/1317 |
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