概括
印度中部山脊的特点是均的低基岩流. 较深的地幔岩石,包括石,在山脊上暴露.
科学领域:
- 地质地质地质地质地质地
- 海洋学 海洋学 海洋学
- 石化学 石化学是一门学科.
背景情况:
- 印度中部山脊是一个中洋山脊系统.
- 了解海洋地和上层地幔的组成对于板块构造学和地幔动力学至关重要.
研究的目的:
- 为了描述沿着印度中部山脊暴露的岩石的组成.
- 为了调查上层地幔岩石在中洋山脊的起源和位置.
主要方法:
- 基岩岩样本的地球化学分析.
- 对加布罗岩石和赫尔佐石岩石样本的石化分析.
主要成果:
- 统一组成的低基岩流覆盖了山脊.
- 在十字骨折中发现了Gabbro,anorthosite和带花石的lherzolite.
- 莱尔佐利特构成了山脊中心的基石,代表了暴露的上层地幔.
结论:
- 印度中部山脊暴露了地球上层地幔的重要部分.
- 断层过程负责将这些深层地幔岩石带到表面.
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