Hostname: page-component-586b7cd67f-l7hp2 Total loading time: 0 Render date: 2024-11-23T09:10:24.154Z Has data issue: false hasContentIssue false

Transmission electron microscopic study of new, regular, mixed-layer structures in calcium-rare-earth fluorocorbonote minerals

Published online by Cambridge University Press:  05 July 2018

Wu Xiuling
Affiliation:
Department of Physics, China University of Geosciences, Wuhan 430074, P.R. China
Meng Dawei
Affiliation:
Department of Physics, China University of Geosciences, Wuhan 430074, P.R. China
Pan Zhaolu
Affiliation:
Department of Physics, China University of Geosciences, Wuhan 430074, P.R. China
Yang Guangming
Affiliation:
Department of Physics, China University of Geosciences, Wuhan 430074, P.R. China
Li Douxing
Affiliation:
Laboratory of Atomic Imaging of Solids, Institute of Metal Research, Academia Sinica, Shenyang 110015, P.R. China

Abstract

Structures of calcium-rare-earth (Ca-RE) fluorocarbonate minerals from southwest China have been investigated using selected area electron diffraction (SAED) and high-resolution transmission electron microscopy (HRTEM). They are described as combinations of layers of bastnäsite-(Ce), CeFCO3 (B layers), and synchysite-(Ce), CeFCO3·CaCO3 (S layers) (Donnay and Donnay, 1953). We report here the discovery of six new, regular, mixed-layer structures in parisite-(Ce) observed using SAED and HRTEM. The symmetry, cell parameters, chemical formulae and stacking of the structural unit layers, etc., were determined for each. The regular, mixed-layer structures are formed by stacking unit layers of bastnäsite-(Ce) and synchysite-(Ce) in varying proportions along the c axis. HRTEM shows that there are different distribution modes for the Ce-F ion layers, the CO3 ion groups between the Ce-F ion layers and the CO3 ion groups between the Ce-F and Ca ion layers. The minerals may be regarded as polymorphs with the same chemical composition and the same spacing of the unit layers, but different arrangements of ion layers in the structural unit layers and different stacking sequences of the structural unit layers.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1998

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Donnay, G. and Donnay, J.D.H. (1953) The crystallography of bastnaesite-(Ce), parisite, roentgenite- (Ce) and synchysite-(Ce). Amer. Mineral., 38, 932–63.Google Scholar
Donnay, G. (1953) Roentgenite-(Ce). A new mineral from Greenland. Amer. Mineral., 38, 868–70.Google Scholar
Ni, Y.X., Hughes, J.M. and Mariano, A.N. (1993) The atomic arrangement of bastnaesite-(Ce), Ce(CO3)F, and structural elements of synchysite-(Ce), roentgenite-( Ce), and parisite-(Ce). Amer. Mineral., 78, 415–8.Google Scholar
Van Landuyt, J. and Amelinckx, S. (1975) Multiple beam direct lattice imaging of new mixed-layer compound of the bastnaesite–synchysite series. Amer. Mineral., 60, 351–8.Google Scholar