Crystal chemistry of the monazite and xenotime structures

Other| February 01, 1995 Crystal chemistry of the monazite and xenotime structures Yunxiang Ni; Yunxiang Ni Miami University, Department of Geology, Oxford, OH, United States Search for other works by this author on: GSW Google Scholar John M. Hughes; John M. Hughes Search for other works by this author on: GSW Google Scholar Anthony N. Mariano Anthony N. Mariano Search for other works by this author on: GSW Google Scholar American Mineralogist (1995) 80 (1-2): 21–26. https://doi.org/10.2138/am-1995-1-203 Article history first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation Yunxiang Ni, John M. Hughes, Anthony N. Mariano; Crystal chemistry of the monazite and xenotime structures. American Mineralogist 1995;; 80 (1-2): 21–26. doi: https://doi.org/10.2138/am-1995-1-203 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyAmerican Mineralogist Search Advanced Search Abstract Monazite and xenotime, the RE(PO4) dimorphs, are the most ubiquitous rare earth (RE) minerals, yet accurate structure studies of the natural phases have not been reported. Here we report the results of high-precision structure studies of both the natural phases and the synthetic RE(PO4) phases for all individual stable rare earth elements.Monazite is monoclinic, P21/n, and xenotime is isostructural with zircon (space group I41/amd). Both atomic arrangements are based on 001 chains of intervening phosphate tetrahedra and RE polyhedra, with a REO8 polyhedron in xenotime that accommodates the heavy lanthanides (Tb–Lu in the synthetic phases) and a REO9 polyhedron in monazite that preferentially incorporates the larger light rare earth elements (La–Gd). As the structure "transforms" from xenotime to monazite, the crystallographic properties are comparable along the 001 chains, with structural adjustments to the different sizes of RE atoms occurring principally in (001).There are distinct similarities between the structures that are evident when their atomic arrangements are projected down 001. In that projection, the chains exist in (100) planes, with two planes per unit cell. In monazite the planes are offset by 2.2 Å along 010, relative to those in xenotime, in order to accommodate the larger light RE atoms. The shift of the planes in monazite allows the RE atom in that phase to bond to an additional O2′ atom to complete the REO9 polyhedron. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.