A type of crust that has been folded to an extreme extent, with the axial surface almost horizontal. It is often seen in areas with significant folds, such as the Alps and the Himalayas. Source: The Selected Edition of the Japanese Language Dictionary About the Selected Edition of the Japanese Language Dictionary Information |
〘名〙 褶曲作用が極度に進み、軸面がほとんど水平に倒れたもの。アルプス山脈やヒマラヤ山脈のような著しい褶曲山脈地域に多く見られる。おしかぶせ。
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