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地幔流体通过柔性下层地的流动:同位素趋势
B Mack Kennedy1, Matthijs C van Soest
1Center for Isotope Geochemistry, Earth Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA 94720, USA. bmkennedy@lbl.gov
地幔液体可以通过由地变形引起的增强透性到达浅层地. 这种以同位素比率表示的过程突出了潜在的地热能源资源.
科学领域:
- 地质化学 地质化学
- 构造学 构造学 构造学 构造学
- 地质物理学 地质物理学
背景情况:
- 地幔液体通过通过柔性下层地的流动,为浅层地提供热量和质量.
- 表面流体中的同位素比率 (3He/4He) 作为地幔衍生流体的标志物.
研究的目的:
- 调查地变形和地幔流体在北方盆地和范围省的上游之间的关系.
- 评估基于同位素特征识别地热能资源的潜力.
主要方法:
- 在北方盆地和范围省的表面流体中分析最小的3He/4He比率.
- 同位素数据与活跃地延伸率和剪切应变率的相关性.
主要成果:
- 观察到3He/4He比率从地到地幔的比率从西到东系统地增加.
- 最高的3He/4He比率与地延伸和剪切应变的最大速率相关.
- 3He/4He中的局部异常表明隐藏的岩活动或深层流体的产生.
结论:
- 活跃的地变形增强了透性,使地幔液体能够进入柔性石化层.
- 同位素比可以识别具有高地热潜力的区域,即使没有显著的岩.
- 变形增强的透性是从地幔转移到地的热量和质量的关键机制.
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