ŽÁČEK, Vladimír, Radek ŠKODA and Petr SULOVSKY. U-Th-rich zircon, thorite and allanite-(Ce) as a main carriers of radioactivity in the highly radioactive ultrapotassic melasyenite porphyry from the Šumava Mts., Moldanubian Zone, Czech Republic. Journal of Geosciences. 2009, vol. 54, No 4, p. 343-354. ISSN 1802-6222.
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Basic information
Original name U-Th-rich zircon, thorite and allanite-(Ce) as a main carriers of radioactivity in the highly radioactive ultrapotassic melasyenite porphyry from the Šumava Mts., Moldanubian Zone, Czech Republic
Authors ŽÁČEK, Vladimír (203 Czech Republic), Radek ŠKODA (203 Czech Republic, guarantor) and Petr SULOVSKY (203 Czech Republic).
Edition Journal of Geosciences, 2009, 1802-6222.
Other information
Original language English
Type of outcome Article in a journal
Field of Study 10500 1.5. Earth and related environmental sciences
Country of publisher Czech Republic
Confidentiality degree is not subject to a state or trade secret
RIV identification code RIV/00216224:14310/09:00028860
Organization unit Faculty of Science
UT WoS 000207803200003
Keywords in English melasyenite porphyry; radioactivity; zircon; thorite; allanite-(Ce); Moldanubicum; Bohemian Massif
Tags International impact, Reviewed
Changed by Changed by: doc. Mgr. Radek Škoda, Ph.D., učo 21802. Changed: 8/4/2010 14:09.
Abstract
A melasyenite porphyry from the vicinity of Kašperské Hory (the Šumava Mts., Moldanubian Zone) shows a high natural radioactivity (K = 4.4-6.1 wt. %, eU = 15-24 ppm, eTh = 38-49 ppm). The most important carriers of U and Th are zircon, thorite, allanite-(Ce) and scarce monazite. Most of the zircon and thorite grains are altered by post-magmatic processes of due to which especially the zircon shows a large degree of chemical variability.
Links
KJB301630801, research and development projectName: Interakce metamiktních minerálů s hydrotermálnímy fluidy a její význam geologickém prostředí
Investor: Academy of Sciences of the Czech Republic, The interaction of metamict minerals and hydrothermal fluids and its significance in the geological environment
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