地層内部で大規模な液状化・流動化が起り、地下から周囲の岩石を取り込みながら上昇してできたダイアピル岩体です。このダイアピルには、牟婁付加体に由来する泥岩の角礫が含まれていて、ダイアピル岩体が牟婁付加体から上昇して熊野層群の内部に注入したことがわかります。

It is a diapir body formed by large-scale liquefaction and fluidization inside the stratum and rising while taking in surrounding rocks from underground. It can be seen that this diapir contains mudstone pebbles derived from the mudstone accretionary prism, and that the diapir accretionary prism rises from the accretionary prism and is injected into the Kumano Group.
google t.

うえもり　う 2022/01/20(Thu) 15:50 No.129

Re: 太地町・マップ６７：E2　伴待瀬海岸のダイアピル

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