Abstract:Dolerite occurs as blocks within serpentinite in the Kurosegawa Belt, located between the Northern and Southern Chichibu belts on Shima Peninsula, Mie Prefecture, Southwest Japan. On the peninsula, this dolerite is considered as a significant component of the Kurosegawa Paleozoic Rocks that define the Kurosegawa Belt. However, dolerite itself is not necessarily the component because it also appears, to a minor extent, in Jurassic accretionary complexes distributed across the Northern and Southern Chichibu belt… Show more
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