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島根大学教育学部紀要. 自然科学 Volume 23 Issue 1
published_at 1989-07-25
大山元谷の河床礫中に見られる片麻岩状捕獲岩
Gneissic Rocks Found as Xenoliths in Dacite Gravels from Mt. Daisen
Miura Kiyoshi
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Present author recently found gneissic xenoliths in dacite gravels of Motodani, westward valley of Mt.Daisen.
From the results of petrological studies, these gneissic rocks are judged to be the rocks of Hida-Oki metamorphic belt.
It is important problem to know not only the basement rocks of Mt.Daisen but also south extremity of Hida-Oki metamorphic belt.
The discovery of gneissic xenoliths from Mt.Daisen sugests the existence of similar materials to those gneissic xenolithsin considerable amounts under Mt.Daisen.
From the results of petrological studies, these gneissic rocks are judged to be the rocks of Hida-Oki metamorphic belt.
It is important problem to know not only the basement rocks of Mt.Daisen but also south extremity of Hida-Oki metamorphic belt.
The discovery of gneissic xenoliths from Mt.Daisen sugests the existence of similar materials to those gneissic xenolithsin considerable amounts under Mt.Daisen.
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