イザナギプレート
1. Izanagi PlateThe Izanagi Plate was an ancient tectonic plate, which began subducting beneath the Okhotsk section of the North American Plate during 130 - 100 Ma. The rapid plate motion of the Izanagi Plate caused the northward drift of north-west Japan and the outer zone of south-west Japan. Sanbagawa metamorphic rocks were formed in the eastern margin of the drifting land mass, while Abukuma metamorphic rocks were formed in its western margin.
Read “Izanagi Plate” on English Wikipedia
Read “イザナギプレート” on Japanese Wikipedia
Read “Izanagi Plate” on DBpedia
Read “Izanagi Plate” on English Wikipedia
Read “イザナギプレート” on Japanese Wikipedia
Read “Izanagi Plate” on DBpedia
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