ČOBIČ, Andrea, Vladimir BERMANEC, Nenad TOMAŠIČ and Radek ŠKODA. The hydrothermal recrystallization of metamict allanite-(Ce). Canadian Mineralogist. 2010, vol. 48, No 3, p. 513-521. ISSN 0008-4476.
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Basic information
Original name The hydrothermal recrystallization of metamict allanite-(Ce)
Authors ČOBIČ, Andrea (191 Croatia), Vladimir BERMANEC (191 Croatia), Nenad TOMAŠIČ (191 Croatia) and Radek ŠKODA (203 Czech Republic, guarantor).
Edition Canadian Mineralogist, 2010, 0008-4476.
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 Canada
Confidentiality degree is not subject to a state or trade secret
Impact factor Impact factor: 1.289
RIV identification code RIV/00216224:14310/10:00040621
Organization unit Faculty of Science
UT WoS 000280414600005
Keywords in English allanite-(Ce); metamictization; hydrothermal recrystallization; X-ray diffraction; granitic pegmatite
Tags International impact, Reviewed
Changed by Changed by: doc. Mgr. Radek Škoda, Ph.D., učo 21802. Changed: 12/11/2010 12:09.
Abstract
Samples of metamict allanite-(Ce) originating from granite pegmatites were recrystallized by heating in air and under hydrothermal conditions. Recrystallization in air resulted in partial recovery of the crystal structure at 650oC. Heating at higher temperatures resulted in decomposition of the allanite structure to a multiphase assemblage containing hematite, cerianite, feldspar, britholite and thorianite. To our knowledge, this is the first report of thorianite as a breakdown product of allanite in literature. The collapse of the structure is mainly related to the removal of structural H2O. Recrystallization under hydrothermal conditions yielded a more rapid and complete recovery of the structure at lower temperatures, without the appearance of additional phases. The stability of the allanite structure during hydrothermal recrystallization is related to the retention of OH- groups, available because of the aqueous environment of recrystallization. Also, H2O promotes a more rapid and efficient recrystallization due to the enhanced diffusion of cations. Crystallite size and strain calculation also record evidence of the recovery of the structure of damaged allanite.
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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