ルーマニアの地震性 - 沈みゆく石層の証拠
1Department of Geodesy and Geophysics, University of Cambridge.
Nature
|December 19, 1970
まとめ
ルーマニアの地震は,カルパトの弧の下の沈没する石層を示唆しています. この地震活動は,東南ヨーロッパのプレート構造と一致し,熱,重力,地質データによって支持されています.
科学分野:
- 地質物理学 地質物理学とは地質物理学です.
- 地震学 地震学とは
- プレート・テクトニクス (プレート・テクトニクス)
背景:
- 中程度の深さの地震の背後にあるメカニズムを理解することは,地震の危険性評価に不可欠です.
- カルパチア弧地域は,複雑な地質学と構造学的な活動を示しています.
研究 の 目的:
- ルーマニアにおける地震の分布と特徴を分析する.
- この地域の中間地震の根本的な原因を調査する.
主な方法:
- ルーマニアからの地震データのレビューと分析.
- 熱と重力の異常を調査する.
- Petrological and tectonic feature analysis. 石油学および地形学的な特徴分析. 石油学および地形学的な特徴分析. 石油学および地形学的な特徴分析. 石油学および地形学的な特徴分析.
主要な成果:
- 地震の分布は,カルパテの弧の下の地下化または沈没する石層を示しています.
- 熱力,重力,地質学,地質学データは,地震の発見を裏付けている.
結論:
- この発見は,プレートテクトニクス理論を東南ヨーロッパに適用することを支持する.
- この研究は,ルーマニアの地震性を推進する地動力学的プロセスについての洞察を提供します.
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