To clarify the signatures and provenance evolution of Jurassic accretionary complexes, we studied the petrographic features and bulk chemistry of sandstones in the Southern Chichibu Belt and northern margin of the Shimanto Belt, eastern Kyushu, and in the Tamba Takami and Itaya, 1996Murata, 1981 Fig. 4 Takami and Itaya 1996 Takami and Itaya, Huang et , 1971 , 1975;Adachi, 1976;, 1984; 1989 1989
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