2005
DOI: 10.5575/geosoc.111.361
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CHIME zircon age of garnet-granite from the Naguri Fault Zone, Kanto Mountains, central Japan

Abstract: The Chichibu Composite Terrane hereafter, Chichibu Terrane consists of the North and South Chichibu Belts with the Kurosegawa Terrane in between. The Kurosegawa Terrane represents typically a serpentinite mélange zone containing peculiar rocks which are exotic to the Jurassic to Early Cretaceous Chichibu accretionary complex hereafter, Chichibu Complex and is characteristically associated with the Cretaceous forearc basin deposits. In the Kanto Mountains Fig. 1 , the Sanchu Graben is generally accepted as the … Show more

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