25亿年前的板块构造:在南印度科拉尔的证据
概括
印度的古老科拉石带揭示了不同的地质地形. 有证据表明,板块构造在25亿年前就在地球上活跃.
科学领域:
- 地质地质地质地质地质地
- 构造学 构造学 构造学 构造学
- 地球科学 地球科学 地球科学
背景情况:
- 印度南部的古老科拉石带是一个复杂的线区域.
- 它具有多个gneiss和两岩地形,具有独特的地质历史.
研究的目的:
- 为了调查科拉尔页岩带的积累历史.
- 确定地形对立的时间及其对早期地球构造学的影响.
主要方法:
- 对两岩的不兼容元素和同位素特征的分析.
- 科拉尔页岩带的地质绘图和结构分析.
主要成果:
- 来自带的不同侧面的两岩石显示出不同的地化学特征,表明了不同的地幔来源.
- 由于压缩和剪切,地形的并置发生在2.5亿至2.4亿年前.
结论:
- 科拉尔页岩带的积累历史可与现代的融合边缘相提并论.
- 这表明,板块构造在25亿年前就在地球上运作.
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