The Tamba Terrane exposed in Southwest Japan is composed mainly of basalt, limestone, chert, mudstone and sandstone, and is characterized by a chaotic mixture of these rocks; i.e., slabs of basalt, limestone, chert, mudstone and sandstone are embedded in pelitic mixed rock. Few biostratigraphical studies in the Nishizu district, located at a southwestern part of Fukui Prefecture, have previously been appeared and some of them described the occurrence of Permian, Triassic and Jurassic radiolarians. However, age of elastic rocks such as mudstone and siliceous mudstone in this district are still unknown, because these radiolarians were yielded only from cherts. Through the present work, about 430 rock samples of chert, siliceous mudstone and mudstone were collected to extract radiolarians from the Nishizu district and its adjacent area, and Triassic and Jurassic radiolarians were detected from 15 samples. As a result, they can give the rocks additional ages as follows; Triassic, Early and Middle Jurassic for cherts, Late Triassic and Jurassic for siliceous mudstones, and Early to Middle Jurassic for mudstones.
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