Now showing items 1-1 of 1
Chloritoid-bearing basic schists from the Sanbagawa metamorphic belt, central Shikoku: their petrologic significance and tectonic implications
(Journal of Mineralogical and Petrological Sciences, Volume 100, page 43-54, 2005, 2005)
Chloritoid- and taramite-bearing basic schists occur on the streambed at Ikadadu in the garnet zone of the Sanbagawa metamorphic belt, central Shikoku. Their major constituent phases are chloritoid, taramite, chlorite, ...