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密度流

2 件の記事

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重力流（密度流）のメカニズムと自然界・建築環境への影響

重力流密度流流体力学ブシネスク近似
2026年8月12日続きを読む →
Turbidites are deposited in the deep ocean troughs below the continental shelf, or similar structures in deep lakes, by underwater avalanches which slide down the steep slopes of the continental shelf edge. When the material comes to rest in the ocean trough, it is the sand and other coarse material which settles first followed by mud and eventually the very fine particulate matter. It is this sequence of deposition that creates the Bouma sequences that characterize these rocks.

タービダイトのメカニズムと地質学的意義深海堆積物の構造と形成

タービダイト混濁流ブーマ・シーケンス深海堆積物
2026年8月11日続きを読む →