海洋地积累的石约会
C Johan Lissenberg1, Matthew Rioux, Nobumichi Shimizu
1Equipe de Géosciences Marines, Institut de Physique du Globe de Paris, 4 Place Jussieu, 75252 Paris Cedex 05, France. lissenbergcj@cardiff.ac.uk
概括
地球地主要是在中洋山脊上形成的. 新的石年代测定揭示了在维玛断裂区的正常地生长模式和浅层融化输送,这表明沿着缓慢扩散的山脊沿着两种不同的地积累模式.
科学领域:
- 地质地质地质地质地质地
- 地质物理学 地质物理学
- 海洋学 海洋学 海洋学
背景情况:
- 地球地主要在中洋山脊上形成.
- 了解地形成过程是板块构造学的关键.
- 缓慢扩散的山脊占地球海洋地的很大一部分.
研究的目的:
- 为了研究维玛骨折区域的地生长模式.
- 为了确定海洋布的石结晶的时间尺度.
- 为了确定沿着缓慢扩散的山脊形成的不同地积模式.
主要方法:
- 的高精度-测定时间.
- 来自维玛骨折区的骨样本的分析.
- 整合新的数据与以前的约会研究.
主要成果:
- 维玛裂区的地表现出高度规律的生长模式.
- 证据表明在地积过程中提供浅层融.
- 海洋浮动岩石中的结晶发生在9万到23万5千年前.
结论:
- 沿着缓慢扩散的山脊存在两种不同的地增殖模式.
- 正常的地生长和浅层融化供应是该地区的特点.
- 石约会为海洋地的时间演变提供了洞察力.
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