中海基岩化学和距离大陆之间的相关性
1Laboratoire des Geosciences Marines, IPGP-Université Denis Diderot, 4, Place Jussieu, 75252 Paris Cedex 05, France. humler@ipgp.jussieu.fr
Nature
|October 11, 2002
概括
大陆边缘影响地球地幔温度. 中洋脊基岩化学揭示了地幔与大陆相距的显著冷却,提供了关于地幔对流和热结构的关键数据.
科学领域:
- 地质物理学 地质物理学
- 地质化学 地质化学
- 地球科学 地球科学 地球科学
背景情况:
- 了解地球地幔对流需要解决温度变化.
- 假设包括放射性衰变和核心热流.
- 大陆的热特性可能会影响地幔对流,但数据有限.
研究的目的:
- 为了研究大陆质量对地幔温度的影响.
- 收集定量数据来测试地幔对流的模型.
主要方法:
- 检查了中海基石的化学成分.
- 与大陆边缘的距离相关的玄武岩化学 (反映地幔温度).
主要成果:
- 在俯冲区或热点附近没有发现相关性.
- 在大西洋和印度洋的中洋岩中观察到显著的相关性.
- 地幔从大陆边缘每公里冷却0.05至0.1°C.
结论:
- 大陆质量相对于山脊的位置会影响大规模的地幔热结构.
- 提供了大陆-地幔热相互作用的定量证据.
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