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- W24993001 abstract "The radioactivity of rocks chiefly being developed in the boundsries of the so-called breaking-zone of the Perzhsn intrusive in Sushchano-Perzhan has been studied. The limitation of heightened radioactivity to filmy and ochreous formations of grayish-dark, greenish-yellow and brown color in the fissures in the granite of Perzhan has been ascertained. If the uranium content in granite is on the average 25 x 10>s-/sup > /rcent, it varies in the filmy and ochreous formations from 37 x 10>s-/sup > /rcent to 72 x 10>s-/sup > /rcent. Among the latter the most radioactive are grayishdark coatings, often with sulfides and fluorite, which, as a rule, flll up the steeply dropping flssures in the granite. A prevailing uranium content (Th/U = 0.66) is typical, being connected with minerals of the group of uranium oxides. The Th/U ratio in ochreous fomations of greenish-yellow and brown color is on the average 1.5. Their radioactivity is conditioned by autunite, ursnocircite, clarkeite snd soddyite. A heightened content of radioelements (U 24 x 10>s-/sup > / percent and Th, 10 x 10>s-/sup > / rcent) has been fixed in the Perzhan granite on the area of Perga-Rudnya Perzhanskaya where the processes of hydrothermal quartzization are most intensively developed.more » This is indicative of the considerable role of hydrothermal processes in the introduction of radioelements into rocks of the Perzhan intrusive. (auth)« less" @default.
- W24993001 created "2016-06-24" @default.
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- W24993001 date "1961-01-01" @default.
- W24993001 modified "2023-09-26" @default.
- W24993001 title "ON THE RADIOACTIVITY OF ROCKS OF THE PERZHAN INTRUSIVE COMPLEX" @default.
- W24993001 hasPublicationYear "1961" @default.
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