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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| Formatua: | Artigo |
| Hizkuntza: | Inglês |
| Argitaratua: |
A.N. Zavaritsky Institute of Geology and Geochemistry
2020-08-01
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| Saila: | Литосфера |
| Gaiak: | |
| Sarrera elektronikoa: | https://www.lithosphere.ru/jour/article/view/1317 |
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