APPLICATION OF ANALYTICAL ELECTRON-MICROSCOPY TO THE STUDY OF RADIATION-DAMAGE IN THE COMPLEX OXIDE MINERAL ZIRCONOLITE

An AEM ratio technique for the analysis of 25 elements in finely zoned natural zirconolite was used in conjunction with electron diffraction and imaging techniques to examine the effects of alpha-decay damage o n zirconolites from Bergell, Switzerland-Italy and Adamello, northern Italy. Comparison of AEM and EPMA results confirms that the AEM techni que can be used to obtain accurate information on the chemical formula of zirconolite. The TEM images and diffraction patterns in this study are analogous to those of previous authors. They support the proposit ion that radiation damage ingrowth can be adequately described by the accumulation and overlap of isolated alpha-recoil collision cascades, producing progressively larger amorphous domains. Careful determinatio n of Th and U contents by AEM gives an accurate indication of the dose range of the crystalline-amorphous transformation. For the samples fr om Bergell and Adamello, the transformation occurs over a dose range o f 0.05 x 10(16) to just over I x 10(16) alpha/mg, consistent with stud ies of synthetic zirconolite doped with Pu-238 Or Cm-244. The Bergell zirconolites all exhibited diffraction patterns characteristic of the zirconolite-2M. Those grains containing REE and Th+U contents up to si milar to 0.1 and similar to 0.03 atoms per formula unit, respectively, exhibit a high level of crystallographic perfection. While those grai ns containing similar to 0.2 REE and 0.06 Th+U atoms per formula unit, exhibit twinning and stacking disorder. (C) 1997 Elsevier Science Ltd .