地球上层地幔底部水性融的稳定性
Tatsuya Sakamaki1, Akio Suzuki, Eiji Ohtani
1Department of Earth and Planetary Material Sciences, Tohoku University, Sendai 980-8578, Japan.
Nature
|January 13, 2006
概括
水性岩可能在410公里不连续度以上保持稳定. 这一发现支持地球上层地幔中低速度区域的融化存在,解释了地震异常.
科学领域:
- 地质物理学 地质物理学
- 矿物物理 矿物物理
- 石化学 石化学是一门学科.
背景情况:
- 地震观测揭示了地球上层地幔410公里不连续的上方低速度和高衰减区域.
- 这些异常表明融的存在,但水性融在这些深度的行为是未知的.
研究的目的:
- 在高压下实验性地确定水性玄武岩融的密度.
- 为了评估410公里不连续度以上水性融的引力稳定性.
主要方法:
- 进行了高压实验,以测量水性玄武岩融的密度.
- 分析了数据,以推断地幔过渡区深度的融化稳定性.
主要成果:
- 水性玄武岩融的密度在压力下受到限制.
- 结果表明,含水性岩可以在410公里不连续度以上保持引力稳定.
结论:
- 在410公里不连续度以上部分融化形成的水性岩可能是稳定的.
- 这种稳定性支持了化存在解释上层地幔地震异常的假设.
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