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Contents of potassium, uranium and thorium were measured using a laboratory gamma–ray spectrometer in more then two thousand samples of Upper Devonian to Lower Carboniferous siliciclastic flysch sediments outcropping on the easternmost margin of the Bohemian Massif (mainly in the Drahany Mts. and Nizký Jesenik Mts.). Studied rocks belong to eight formations: Protivanov Fm., Rozstani Fm., Myslejovice Fm., Mohelnice Fm., Andělska Hora Fm., Horni Benesov Fm., Moravice Fm. and Hradec–Kyjovice Fm. Conglomerates (incl. gravelites), various types of psammites (mainly graywackes), siltstones, silty shales and clay shales occur in all mentioned formations. Quartzites and phyllites dominated in the source zone of clastic sediments of Mohelnice Fm. and Andělska Hora Fm., therefore K, U and Th contents in siliciclastic sediments of the both formations are correspondingly low. Relatively high radioactivity of sediments belonging to remaining six formations suggests a significant contribution of acid or intermediate magmatic rocks in the source zone of clastic material.

PŘIROZENÁ RADIOAKTIVITA KULMSKÝCH SEDIMENTŮ NA VÝCHODNÍM OKRAJI ČESKÉHO MASIVU