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砂岩中の火炎構造 上位層の荷重による下位層の変形のあらわれ 前期鮮新世（約600万年前） 柏崎市 #地層 #地学 #地質
A flame structure in amalgamated turbidite layers, due to plastic deformation by loading from the overlying layer right after the deposition. Early Pliocene, Kashiwazaki city, Niigata, Japan.
