1887

Abstract

There was a uplifted land that existed between the Palaeo-Ural Ocean and Pachelma trough on the South-Eastern margin of the Russian craton during the Late Froterozoic and Early Paleozoic.

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/content/papers/10.3997/2214-4609.201408474
1998-06-08
2021-07-31
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201408474
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