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地殻均衡

2 件の記事

Airy isostasy, in which a constant-density crust floats on a higher-density mantle, and topography is determined by the thickness of the crust.

アイソスタシー(地殻均衡)の仕組みと地球物理学的モデル

アイソスタシー地殻均衡エアリーモデルプラットモデル
A model of present-day mass change due to post-glacial rebound and the reloading of the ocean basins with seawater. Blue and purple areas indicate rising due to the removal of the ice sheets. Yellow and red areas indicate falling as mantle material moved away from these areas in order to supply the rising areas, and because of the collapse of the forebulges around the ice sheets.

氷河後リバウンド地球の地殻がゆっくりと復元するメカニズム

氷河後リバウンド地殻均衡アイソスタシー氷河期