End-Permian Convergent Zone along the Nortern Margin of Kurosegawa Landmass and its Products in Cetral Shikoku, Southwest Japan

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The northern subbelt of the Chichibu Belt, Southwest Japan, retains records of tectonic evolution of the Late Paleozoic and Mesozoic ocean basin developed on the north of the ancient Kurosegawa Landmass (arc or microcontinent). The pre-Cretaceous edifice of this subbelt is composed of two tectono-stratigraphic units, namely the Paleozoic Complex (latest Permian) just on the north of the Kurosegawa Tectonic Zone and the Mesozoic Complex (Jurassic) in the northern half of the subbelt....

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