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The Inagawa Complex, located in Kawanishi City, Hyogo Prefecture, southwestern Japan, is interpreted as a late Permian subduction-related accretionary complex of the Ultra-Tamba Terrane. The complex contains a conglomerate bed, with clasts consisting predominantly of felsic volcanic rocks, serpentinite, and schist, with subordinate amounts of granite, basalt, and sedimentary rock (chert and mudstone, containing late Paleozoic radiolarians). The provenance of the conglomerate is inferred to be a volcanic arc, where volcanic rocks overlay an accretionary complex, sedimentary rocks, metamorphic rocks, and granite. Serpentine grains contain spinel crystals that are unaltered in their cores and exhibit highly irregular shapes resembling so-called “dancing spinel”, which are characteristic of mantle peridotites of the early Paleozoic Oeyama ophiolite. Geochemical analysis of the spinel crystals (Cr#50–51 and Cr#42) confirms that they originate from the Oeyama ophiolite. The discovery of serpentinite from the Oeyama ophiolite in the late Permian subduction-related accretionary complex of the Ultra-Tamba Terrane suggests that the Oeyama ophiolite was exposed in the forearc area of the Permian “Maizuru (Yakuno) arc”, which was floored predominantly by oceanic crust of the Permian Yakuno ophiolite.