概括
一个不寻常的海底山脉揭示了深海上层地幔岩石,升起超过2公里. 这一地质特征是地幔上升和沿断裂区的构造活动造成的.
科学领域:
- * * 海洋地质学
- * 石化学 石化学
- * 构造学 构造学 构造学
背景情况:
- * 在欧文断裂区和中印度山脊交叉点附近的异常地形高处暴露了超级岩石.
- *这些岩石,包括蛇形状的旋石,哈兹堡石和沙丘石,缺乏累积质地.
研究的目的:
- * 调查海洋上层地幔暴露块的起源和升起机制.
- *从地形高处分析超级岩石的岩石学和矿物化学.
主要方法:
- * 对地形高地的实地观测.
- * 超岩样本的纹理分析.
- *对橄素,素和螺旋晶体进行矿物化学分析.
主要成果:
- * 超级岩石起源于海洋石层至少25公里的深度.
- * 在上游过程中观察到部分再平衡和再结晶的证据.
- *数据显示上层地幔的升起块,而不是典型的海洋地部分.
结论:
- *暴露的超级岩石代表了海洋上层地幔的重要块.
- * 两个阶段的过程,包括地幔上升和断裂区构造上升,解释了大量的垂直移位.
- * 沿断裂区域的升起速度估计约为每年1毫米.
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