1887
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Abstract

A system of continental rifts and troughs, which came into existence in the Late Riphean - Vendian and is particularly divergent in the cast of the East-European Craton, only partially precoursed the contours of sedimentary basins originating their in the Late Palaeozoic.

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/content/papers/10.3997/2214-4609.201408063
1999-06-07
2024-04-25
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201408063
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