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The Iratsu epidote amphibolite mass is a metamorphosed layered gabbro, which has mineralogy of the albite-epidote amphibolite fades in the facies series of the Sanbagawa metamorphism (Banno et al., 1976). Lime stone occurs frequently in the mass, especi ally on the northern slope of the Mt. Gongen-Mt. Jiyoshi-Mt. Futatsudake ridge and also sporadically in other areas. Banno (1964) described that limestone of the Tonaru mass, a similar metamorphosed gabbro near the Bessi mine, has diposide+ grossular assemblage, but details of mine ralogy have not been studied. The author found a limestone having similar skarn mine ralogy from the Oki valley, eastern part of the mass. Petrography of the rock with comments on its genesis will be given below.

Notes on petrography and rock-forming mineralogy. 1. Skarn assemblage in limestone of the Iratsu epidote amphibolite mass, central Shikoku.