Journal of Mineralogical and Petrological Sciences
Online ISSN : 1349-3825
Print ISSN : 1345-6296
LETTERS
Cr-rich allanite-(Ce) in the serpentinite-metapelite reaction layer in the Sanbagawa belt of Nushima, Hyogo Prefecture, Japan
Masaki ENAMITomoko UENOHirokazu MAEKAWA
Author information
JOURNALS FREE ACCESS

2011 Volume 106 Issue 2 Pages 103-108

Details
Abstract

Cr-rich allanite-(Ce) has been found in a reaction layer between the serpentinite lens and the host metapelite of the Sanbagawa metamorphic belt in Nushima, Hyogo Prefecture, Japan. The reaction layer is divided into talc, tremolite, and chlorite zones in order from the inner to the outer regions of the layer. The Cr-rich allanite-(Ce) occurs as fine and spindle-shaped grains of 30-60 μm in length in the tremolite zone, and coexists with tremolite and subordinate amounts of chlorite, titanite, graphite, and zircon. The Cr-rich allanite-(Ce) is enriched in Cr2O3 (0.2-9.0 wt%) and total iron as FeO (6.0-9.0 wt%), with the following Cr-richest formula:

(Ca0.98Na0.01K0.01)1.00(REE0.70Ca0.28Th0.01)0.99(Al1.40Cr0.69Fe2+0.63Fe3+0.11Ti0.09Mg0.07Mn0.03)3.02(Si2.94Al0.06)3.00O12(OH),

where REE includes La = 0.17, Ce = 0.33, Pr = 0.04, Nd = 0.13 and Sm = 0.03 per formula unit. The core part of the Cr-rich allanite-(Ce) is partially enriched in TiO2 of up to 2.3 wt%, suggesting the substitution of (Fe2+,Mg)Ti(Fe3+,Al)-2 in the octahedral sites.

Information related to the author
© 2011 Japan Association of Mineralogical Sciences
Previous article Next article
feedback
Top