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- W1490966650 abstract "The paper presents characteristics of composition, structure and distribution pattern of tuffaceous interbeds of the Mid-Late-Famennian potassic subformation of the Pripyat intracontinental palaeorift (the Pripyat Trough, Belarus). Solid products of volcanic activity found there are proofs of significant volcanism influence/contribution on/to accumulation of salt deposits in the Pripyat Trough. Abundance of clastic material, its granulometric and mineralogical composition and distribu- tion within the sedimentary area affected formation of lithological complexes. Interbeds of tuffaceous clays, occurring at 12 levels of the potassic subformation, suggest that the salt accumulation was ac- companied with the volcanic processes. Pyroclastic rocks are represented by ash particles (morpho- logically well-preserved in some crystal-vitric tuffs), pumice, mineral crystals and lithoclasts." @default.
- W1490966650 created "2016-06-24" @default.
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- W1490966650 date "2010-01-01" @default.
- W1490966650 modified "2023-09-23" @default.
- W1490966650 title "PYROCLASTIC ROCKS IN DEPOSITS OF THE POTASSIC SUBFORMATION OF THE PRIPYAT INTRACONTINENTAL PALAEORIFT" @default.
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