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Updated: Jul 20, 2026

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Evolution of Staircase Structures in Diffusive Convection
Published on: September 5, 2018
チベットの高原の斜めの段階的な上昇と成長
P Tapponnier1, X Zhiqin, F Roger
1Institut de Physique du Globe, 4 Place Jussieu, 75252 Paris, France. tappon@ipgp.jussieu.fr
まとめ
チベット高原はチベット高原です.
科学分野:
- 地質学 地質学 地質学
- プレート・テクトニクス (プレート・テクトニクス)
- ジオダイナミクスは地力学です.
背景:
- チベットの高い高さを説明する2つのモデルがあります:広範囲にわたる地殻の流れまたは石層ブロックの間の局所的な切断です.
- 最近のケノゾイク期の変形,マグマチズム,地震データは,局所的剪定モデルを支持している.
研究 の 目的:
- チベット高地の形成メカニズムを調査する.
- 紀元期の変形,マグマチズム,地震構造を分析する.
主な方法:
- セノゾイク時代の変形パターンの分析.
- マグマ帯の調査と,その年齢の進行.
- 地震構造の解釈. 地震構造の解釈.
- 地殻の加厚とマントルの分離のモデリング.
主要な成果:
- チベットの高原の上昇は,地殻の推力ケインの連続した上昇を含む3段階で行われました.
- 地殻の加厚はマントルの解離に伴い,均一な加厚ではありませんでした.
- 山間流域の沈殿により,それぞれの上昇段階の後,平らな高原が形成された.
- 北向きに若返るマグマ帯は,アジアマントルの北方帯域の下での連続的な沈下を示唆している.
- 斜面沈殿とストライクスリップ断層は,東方と北東方への高原の成長に貢献しました.
結論:
- チベットの高原の形成は,石層ブロック間の時間依存的,局所的な切断によって説明され,均一な粘着性流ではなく,最もよく説明されます.
- 斜面沈殿と滑り分割を含むプレート構造は,高原の発展,特に東方および北東方への拡大において重要な役割を果たしました.
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