Journal Article

PHPPUBDB-18850

http://join2-wiki.gsi.de/foswiki/pub/Main/Artwork/join2_logo100x88.png Recrystallization of metamict allanite

Beirau, T. ; Paulmann, C. ; Bismayer, U. ; DESY

2011
Mineralogical Society of Great Britain and Ireland Twickenham

This record in other databases:      

Please use a persistent id in citations: doi:10.1180/minmag.2011.075.4.2393

Abstract: Allanite is a common accessory mineral in igneous rocks. Allanite becomes metamict over geological time-scales as a result of the alpha-decay of radioactive elements in the crystal structure. This study focuses on the recrystallization of metamict allanite from Savvushka, Russia. The structural recovery produced by annealing was investigated by X-ray powder diffraction, single-crystal synchrotron X-ray diffraction and infrared spectroscopy. A kinetic analysis is presented that shows that the recrystallization process proceeds by at least two different mechanisms.

Keyword(s): Chlorine: analysis (MeSH) ; Water Pollution, Chemical: analysis (MeSH) ; Water Supply (MeSH) ; Chlorine

---

Contributing Institute(s):

1. Experiments with synchrotron radiation (HASYLAB)

Research Program(s):

1. DORIS Beamline F1 (POF2-54G13) (POF2-54G13)

Experiment(s):

1. DORIS Beamline F1 (DORIS III)

Appears in the scientific report 2011
Notes: (c) by the Mineralogical Society of Great Britain and Ireland. Verlags- bzw. Post Referee-Version 2 Jahre gesprerrt (bis August 2013).

---

Database coverage:
; JCR ; No Author Disambiguation ; Thomson Reuters Master Journal List ; Web of Science Core Collection

---