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Abstract

Halokinesis in the Pripyat trough displayed in two salt formations: the Upper Frasnian (Evlanov-Liven) and the Middle Famennian (Lebedyan-Streshin) ones.

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/content/papers/10.3997/2214-4609.201408552
1998-06-08
2024-03-28
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201408552
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