在中国北方的地中回收下大陆地
Shan Gao1, Roberta L Rudnick, Hong-Ling Yuan
1Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an 710069, China. sgao@263.net.cn
Nature
|December 17, 2004
概括
马菲亚的下大陆地沉入了地幔,融化形成了高度的石和石. 这一过程解释了大陆地的演化,并且发生在罗纪晚期的中国北方地中.
科学领域:
- 地质化学 地质化学
- 石化学 石化学是一门学科.
- 构造学 构造学 构造学 构造学
背景情况:
- 大陆地的演变往往是由于地的下层地沉入地幔而解释的.
- 这一过程的直接证据是有限的.
- 阿达基特和花状物与板块融化地幔相互作用有关.
研究的目的:
- 为了调查罗纪晚期岩在中国北方石坑的起源.
- 为下大陆地沉没提供直接证据.
- 为了限制石层移除的时间.
主要方法:
- 对高含量的石,大石和石进行化学和岩石分析.
- 同位素分析 (新和).
- 石约会. 在约会.
主要成果:
- 罗纪晚期的岩显示的特征与部分融化的一致性,即生态石与地幔周石相互作用.
- 这些岩含有遗传的阿凯亚时期的石.
- 同位素组成与下层地的生态石异石重叠.
结论:
- 中国的岩起源于古老的马菲斯下层地,入地幔.
- 在罗纪晚期,下层地的沉没发生在中国北方的地中.
- 这为石质层移除提供了证据.
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