まとめ
中大西洋山脈の断層地帯にある超大質量体からは,浅瀬の石灰岩が明らかになる. これらの地質学的形成は,その後の大西洋開口前に,狭い原大西洋に堆積したことを示唆しています.
科学分野:
- 地質学 地質学 地質学
- 海洋地質学 海洋地質学
- プレート・テクトニクス (プレート・テクトニクス)
背景:
- 上層マントルの超大質量体で構成される横断の山脊は,中大西洋の山脊が赤道断裂地帯を交差する場所で発生します.
- オフセットゾーンのこれらの超大質量体は,異なる地殻板の間の不拡散ブロックとして作用します.
研究 の 目的:
- 地質学的構成と中大西洋山脊の横断超大西洋体の起源を調査する.
- これらの超大質量構造に浅瀬の石灰岩の存在を説明するために.
主な方法:
- ヴェマ断裂地帯の横断的な超大質量体の地質学的調査.
- デトリタル粒 (クォーツ,マイクロクライン,オルトクラース) を含む石灰岩の組成の分析.
主要な成果:
- 直径1mmまでのデトリタル粒を持つ浅瀬の石灰岩は,ヴェマ断裂地帯の超大質量体で発見されました.
- ウルトラマフィック体は,広がる地殻板の内部で,広がらないブロックとして機能します.
結論:
- 石灰岩は,狭くて浅い原始大西洋に堆積した可能性が高い.
- これらの堆積物は,大西洋の膨張に伴い,後に残された.
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