在东太平洋下面的融化运动的限制从230Th-238U失衡上升到230Th-238U失衡
Haibo Zou1, Alan Zindler, Yaoling Niu
1Department of Earth and Space Sciences, University of California at Los Angeles, Los Angeles, CA 90095, USA. hzou@ess.ucla.edu
概括
中洋山脊玄武岩在东太平洋上升处以对称的方式喷发,这表明了大规模的地下融化运输. 这项研究提供了关于远离山脊轴的丰富玄武岩的起源的见解.
科学领域:
- 地质化学 地质化学
- 石化学 石化学是一门学科.
- 海洋地质学海洋地质学
背景情况:
- 中洋脊基岩 (MORBs) 提供了关于地球地幔过程的关键信息.
- 了解离轴火山活动是解读岩运输和分化的关键.
- 之前的研究主要集中在轴上的过程上.
研究的目的:
- 为了调查基岩融的起源和运输,远离东太平洋上升.
- 为了分析230Th-238U在离轴玄武岩中的不平衡.
- 为了限制不兼容的元素丰富的中海脊基岩 (EMORB) 的石化.
主要方法:
- 在玄武岩样本中分析230Th-238U不平衡.
- 正常的中海脊基岩石 (NMORBs) 和EMORBs的地化学特征.
- 地质地图绘制和采样火山岩在与山脊轴的不同距离.
主要成果:
- 观察到NMORB和EMORB的近对称喷发距离轴外20公里.
- 有证据表明,NMORB的大规模地下横向输送每年以19-21厘米的速度融化.
- 确定了离轴EMORB的明显地质化学特征.
结论:
- 地下融化运输在离轴火山活动中起着重要作用.
- 在轴外发现的EMORB具有独特的石油遗传历史.
- 这些发现挑战了传统的海洋中山脊岩的模型.
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