まとめ
地球上の海殻は,1億1,000万年に1度リサイクルされます. 大陸の積層率は年間3.0立方キロメートルに達し,大陸の陸地量を年間1.35立方キロメートル増加させる可能性がある.
科学分野:
- 地質学 地質学 地質学
- 地質物理学 地質物理学とは地質物理学です.
- 海洋学 海洋学とは
背景:
- 海洋の地殻は,絶えず生成され,リサイクルされています.
- 沈着プロセスは,潜水地帯への物質移転において重要な役割を果たします.
研究 の 目的:
- シアリック物質の形成と沈殿物の蓄積の速度を定量化するために.
- サブドクションプロセスに基づく大陸積層と純成長率を推定する.
主な方法:
- グローバルな海洋の地殻物質の分析.
- 堆積物の流入速度 (地質的および生物学的) の推定.
- サブドクションゾーンへの物質移動のモデリング.
主要な成果:
- 潜在的シアリック物質形成率: 1.35 km3/年.
- ヘミペラジック火山沈殿物の蓄積: 0.05 km3/年.
- 地質性および生体性沈殿物の流入:年間1.65 km3/年.
- 推定大陸積層速度:最大3.0km3/年.
- コンチネンタル・成長の潜在 neto: 1.35 km3/年.
結論:
- サブドクションゾーンは,大陸の成長にとって重要な場所です.
- 堆積物の流入と地殻の循環は,大陸の収縮に寄与する.
- 地球の大陸は,これらの地質学的プロセスにより,純成長率を示しています.
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